[2259] | 1 | """Class Domain - |
---|
| 2 | 2D triangular domains for finite-volume computations of |
---|
| 3 | the shallow water wave equation. |
---|
| 4 | |
---|
| 5 | This module contains a specialisation of class Domain from module domain.py |
---|
| 6 | consisting of methods specific to the Shallow Water Wave Equation |
---|
| 7 | |
---|
| 8 | |
---|
| 9 | U_t + E_x + G_y = S |
---|
| 10 | |
---|
| 11 | where |
---|
| 12 | |
---|
| 13 | U = [w, uh, vh] |
---|
| 14 | E = [uh, u^2h + gh^2/2, uvh] |
---|
| 15 | G = [vh, uvh, v^2h + gh^2/2] |
---|
| 16 | S represents source terms forcing the system |
---|
| 17 | (e.g. gravity, friction, wind stress, ...) |
---|
| 18 | |
---|
| 19 | and _t, _x, _y denote the derivative with respect to t, x and y respectively. |
---|
| 20 | |
---|
| 21 | The quantities are |
---|
| 22 | |
---|
| 23 | symbol variable name explanation |
---|
| 24 | x x horizontal distance from origin [m] |
---|
| 25 | y y vertical distance from origin [m] |
---|
| 26 | z elevation elevation of bed on which flow is modelled [m] |
---|
| 27 | h height water height above z [m] |
---|
| 28 | w stage absolute water level, w = z+h [m] |
---|
| 29 | u speed in the x direction [m/s] |
---|
| 30 | v speed in the y direction [m/s] |
---|
| 31 | uh xmomentum momentum in the x direction [m^2/s] |
---|
| 32 | vh ymomentum momentum in the y direction [m^2/s] |
---|
| 33 | |
---|
| 34 | eta mannings friction coefficient [to appear] |
---|
| 35 | nu wind stress coefficient [to appear] |
---|
| 36 | |
---|
| 37 | The conserved quantities are w, uh, vh |
---|
| 38 | |
---|
| 39 | |
---|
| 40 | For details see e.g. |
---|
| 41 | Christopher Zoppou and Stephen Roberts, |
---|
| 42 | Catastrophic Collapse of Water Supply Reservoirs in Urban Areas, |
---|
| 43 | Journal of Hydraulic Engineering, vol. 127, No. 7 July 1999 |
---|
| 44 | |
---|
| 45 | |
---|
| 46 | Ole Nielsen, Stephen Roberts, Duncan Gray, Christopher Zoppou |
---|
| 47 | Geoscience Australia, 2004 |
---|
| 48 | """ |
---|
| 49 | |
---|
| 50 | #Subversion keywords: |
---|
| 51 | # |
---|
| 52 | #$LastChangedDate: 2006-01-13 16:43:01 +1100 (Fri, 13 Jan 2006) $ |
---|
| 53 | #$LastChangedRevision: 2206 $ |
---|
| 54 | #$LastChangedBy: steve $ |
---|
| 55 | |
---|
| 56 | |
---|
| 57 | from domain import * |
---|
| 58 | from region import * |
---|
| 59 | |
---|
| 60 | Generic_Domain = Domain #Rename |
---|
| 61 | |
---|
| 62 | #Shallow water domain |
---|
| 63 | class Domain(Generic_Domain): |
---|
| 64 | |
---|
| 65 | def __init__(self, coordinates, vertices, boundary = None, |
---|
| 66 | tagged_elements = None, geo_reference = None, |
---|
| 67 | use_inscribed_circle=False): |
---|
| 68 | |
---|
| 69 | conserved_quantities = ['stage', 'xmomentum', 'ymomentum'] |
---|
| 70 | other_quantities = ['elevation', 'friction'] |
---|
| 71 | Generic_Domain.__init__(self, coordinates, vertices, boundary, |
---|
| 72 | conserved_quantities, other_quantities, |
---|
| 73 | tagged_elements, geo_reference, use_inscribed_circle) |
---|
| 74 | |
---|
| 75 | from config import minimum_allowed_height, g |
---|
| 76 | self.minimum_allowed_height = minimum_allowed_height |
---|
| 77 | self.g = g |
---|
| 78 | |
---|
| 79 | self.forcing_terms.append(gravity) |
---|
| 80 | self.forcing_terms.append(manning_friction) |
---|
| 81 | |
---|
| 82 | #Realtime visualisation |
---|
| 83 | self.visualiser = None |
---|
| 84 | self.visualise = False |
---|
| 85 | self.visualise_color_stage = False |
---|
| 86 | self.visualise_stage_range = 1.0 |
---|
| 87 | self.visualise_timer = True |
---|
| 88 | self.visualise_range_z = None |
---|
| 89 | |
---|
| 90 | #Stored output |
---|
| 91 | self.store = False |
---|
| 92 | self.format = 'sww' |
---|
| 93 | self.smooth = True |
---|
| 94 | |
---|
| 95 | #Reduction operation for get_vertex_values |
---|
| 96 | from util import mean |
---|
| 97 | self.reduction = mean |
---|
| 98 | #self.reduction = min #Looks better near steep slopes |
---|
| 99 | |
---|
| 100 | self.quantities_to_be_stored = ['stage','xmomentum','ymomentum'] |
---|
| 101 | |
---|
| 102 | |
---|
| 103 | |
---|
| 104 | def initialise_visualiser(self,scale_z=1.0,rect=None): |
---|
| 105 | #Realtime visualisation |
---|
| 106 | if self.visualiser is None: |
---|
| 107 | from realtime_visualisation_new import Visualiser |
---|
| 108 | self.visualiser = Visualiser(self,scale_z,rect) |
---|
| 109 | self.visualiser.setup['elevation']=True |
---|
| 110 | self.visualiser.updating['stage']=True |
---|
| 111 | self.visualise = True |
---|
| 112 | if self.visualise_color_stage == True: |
---|
| 113 | self.visualiser.coloring['stage'] = True |
---|
| 114 | self.visualiser.qcolor['stage'] = (0.0, 0.0, 0.8) |
---|
| 115 | print 'initialise visualiser' |
---|
| 116 | print self.visualiser.setup |
---|
| 117 | print self.visualiser.updating |
---|
| 118 | |
---|
| 119 | def check_integrity(self): |
---|
| 120 | Generic_Domain.check_integrity(self) |
---|
| 121 | |
---|
| 122 | #Check that we are solving the shallow water wave equation |
---|
| 123 | |
---|
| 124 | msg = 'First conserved quantity must be "stage"' |
---|
| 125 | assert self.conserved_quantities[0] == 'stage', msg |
---|
| 126 | msg = 'Second conserved quantity must be "xmomentum"' |
---|
| 127 | assert self.conserved_quantities[1] == 'xmomentum', msg |
---|
| 128 | msg = 'Third conserved quantity must be "ymomentum"' |
---|
| 129 | assert self.conserved_quantities[2] == 'ymomentum', msg |
---|
| 130 | |
---|
| 131 | def extrapolate_second_order_sw(self): |
---|
| 132 | #Call correct module function |
---|
| 133 | #(either from this module or C-extension) |
---|
| 134 | extrapolate_second_order_sw(self) |
---|
| 135 | |
---|
| 136 | def compute_fluxes(self): |
---|
| 137 | #Call correct module function |
---|
| 138 | #(either from this module or C-extension) |
---|
| 139 | compute_fluxes(self) |
---|
| 140 | |
---|
| 141 | def distribute_to_vertices_and_edges(self): |
---|
| 142 | #Call correct module function |
---|
| 143 | #(either from this module or C-extension) |
---|
| 144 | distribute_to_vertices_and_edges(self) |
---|
| 145 | |
---|
| 146 | |
---|
| 147 | #FIXME: Under construction |
---|
| 148 | # def set_defaults(self): |
---|
| 149 | # """Set default values for uninitialised quantities. |
---|
| 150 | # This is specific to the shallow water wave equation |
---|
| 151 | # Defaults for 'elevation', 'friction', 'xmomentum' and 'ymomentum' |
---|
| 152 | # are 0.0. Default for 'stage' is whatever the value of 'elevation'. |
---|
| 153 | # """ |
---|
| 154 | |
---|
| 155 | # for name in self.other_quantities + self.conserved_quantities: |
---|
| 156 | # print name |
---|
| 157 | # print self.quantities.keys() |
---|
| 158 | # if not self.quantities.has_key(name): |
---|
| 159 | # if name == 'stage': |
---|
| 160 | |
---|
| 161 | # if self.quantities.has_key('elevation'): |
---|
| 162 | # z = self.quantities['elevation'].vertex_values |
---|
| 163 | # self.set_quantity(name, z) |
---|
| 164 | # else: |
---|
| 165 | # self.set_quantity(name, 0.0) |
---|
| 166 | # else: |
---|
| 167 | # self.set_quantity(name, 0.0) |
---|
| 168 | |
---|
| 169 | |
---|
| 170 | |
---|
| 171 | # #Lift negative heights up |
---|
| 172 | # #z = self.quantities['elevation'].vertex_values |
---|
| 173 | # #w = self.quantities['stage'].vertex_values |
---|
| 174 | |
---|
| 175 | # #h = w-z |
---|
| 176 | |
---|
| 177 | # #for k in range(h.shape[0]): |
---|
| 178 | # # for i in range(3): |
---|
| 179 | # # if h[k, i] < 0.0: |
---|
| 180 | # # w[k, i] = z[k, i] |
---|
| 181 | |
---|
| 182 | |
---|
| 183 | # #self.quantities['stage'].interpolate() |
---|
| 184 | |
---|
| 185 | |
---|
| 186 | def evolve(self, yieldstep = None, finaltime = None, |
---|
| 187 | skip_initial_step = False): |
---|
| 188 | """Specialisation of basic evolve method from parent class |
---|
| 189 | """ |
---|
| 190 | |
---|
| 191 | #Call check integrity here rather than from user scripts |
---|
| 192 | #self.check_integrity() |
---|
| 193 | |
---|
| 194 | msg = 'Parameter beta_h must be in the interval [0, 1[' |
---|
| 195 | assert 0 <= self.beta_h < 1.0, msg |
---|
| 196 | msg = 'Parameter beta_w must be in the interval [0, 1[' |
---|
| 197 | assert 0 <= self.beta_w < 1.0, msg |
---|
| 198 | |
---|
| 199 | |
---|
| 200 | #Initial update of vertex and edge values before any storage |
---|
| 201 | #and or visualisation |
---|
| 202 | self.distribute_to_vertices_and_edges() |
---|
| 203 | |
---|
| 204 | #Initialise real time viz if requested |
---|
| 205 | if self.visualise is True and self.time == 0.0: |
---|
| 206 | if self.visualiser is None: |
---|
| 207 | self.initialise_visualiser() |
---|
| 208 | |
---|
| 209 | self.visualiser.update_timer() |
---|
| 210 | self.visualiser.setup_all() |
---|
| 211 | |
---|
| 212 | #Store model data, e.g. for visualisation |
---|
| 213 | if self.store is True and self.time == 0.0: |
---|
| 214 | self.initialise_storage() |
---|
| 215 | #print 'Storing results in ' + self.writer.filename |
---|
| 216 | else: |
---|
| 217 | pass |
---|
| 218 | #print 'Results will not be stored.' |
---|
| 219 | #print 'To store results set domain.store = True' |
---|
| 220 | #FIXME: Diagnostic output should be controlled by |
---|
| 221 | # a 'verbose' flag living in domain (or in a parent class) |
---|
| 222 | |
---|
| 223 | #Call basic machinery from parent class |
---|
| 224 | for t in Generic_Domain.evolve(self, yieldstep, finaltime, |
---|
| 225 | skip_initial_step): |
---|
| 226 | #Real time viz |
---|
| 227 | if self.visualise is True: |
---|
| 228 | self.visualiser.update_all() |
---|
| 229 | self.visualiser.update_timer() |
---|
| 230 | |
---|
| 231 | |
---|
| 232 | #Store model data, e.g. for subsequent visualisation |
---|
| 233 | if self.store is True: |
---|
| 234 | self.store_timestep(self.quantities_to_be_stored) |
---|
| 235 | |
---|
| 236 | #FIXME: Could maybe be taken from specified list |
---|
| 237 | #of 'store every step' quantities |
---|
| 238 | |
---|
| 239 | #Pass control on to outer loop for more specific actions |
---|
| 240 | yield(t) |
---|
| 241 | |
---|
| 242 | def initialise_storage(self): |
---|
| 243 | """Create and initialise self.writer object for storing data. |
---|
| 244 | Also, save x,y and bed elevation |
---|
| 245 | """ |
---|
| 246 | |
---|
| 247 | import data_manager |
---|
| 248 | |
---|
| 249 | #Initialise writer |
---|
| 250 | self.writer = data_manager.get_dataobject(self, mode = 'w') |
---|
| 251 | |
---|
| 252 | #Store vertices and connectivity |
---|
| 253 | self.writer.store_connectivity() |
---|
| 254 | |
---|
| 255 | |
---|
| 256 | def store_timestep(self, name): |
---|
| 257 | """Store named quantity and time. |
---|
| 258 | |
---|
| 259 | Precondition: |
---|
| 260 | self.write has been initialised |
---|
| 261 | """ |
---|
| 262 | self.writer.store_timestep(name) |
---|
| 263 | |
---|
| 264 | |
---|
| 265 | #=============== End of Shallow Water Domain =============================== |
---|
| 266 | |
---|
| 267 | |
---|
| 268 | |
---|
| 269 | #Rotation of momentum vector |
---|
| 270 | def rotate(q, normal, direction = 1): |
---|
| 271 | """Rotate the momentum component q (q[1], q[2]) |
---|
| 272 | from x,y coordinates to coordinates based on normal vector. |
---|
| 273 | |
---|
| 274 | If direction is negative the rotation is inverted. |
---|
| 275 | |
---|
| 276 | Input vector is preserved |
---|
| 277 | |
---|
| 278 | This function is specific to the shallow water wave equation |
---|
| 279 | """ |
---|
| 280 | |
---|
| 281 | from Numeric import zeros, Float |
---|
| 282 | |
---|
| 283 | assert len(q) == 3,\ |
---|
| 284 | 'Vector of conserved quantities must have length 3'\ |
---|
| 285 | 'for 2D shallow water equation' |
---|
| 286 | |
---|
| 287 | try: |
---|
| 288 | l = len(normal) |
---|
| 289 | except: |
---|
| 290 | raise 'Normal vector must be an Numeric array' |
---|
| 291 | |
---|
| 292 | assert l == 2, 'Normal vector must have 2 components' |
---|
| 293 | |
---|
| 294 | |
---|
| 295 | n1 = normal[0] |
---|
| 296 | n2 = normal[1] |
---|
| 297 | |
---|
| 298 | r = zeros(len(q), Float) #Rotated quantities |
---|
| 299 | r[0] = q[0] #First quantity, height, is not rotated |
---|
| 300 | |
---|
| 301 | if direction == -1: |
---|
| 302 | n2 = -n2 |
---|
| 303 | |
---|
| 304 | |
---|
| 305 | r[1] = n1*q[1] + n2*q[2] |
---|
| 306 | r[2] = -n2*q[1] + n1*q[2] |
---|
| 307 | |
---|
| 308 | return r |
---|
| 309 | |
---|
| 310 | |
---|
| 311 | |
---|
| 312 | #################################### |
---|
| 313 | # Flux computation |
---|
| 314 | def flux_function_central(normal, ql, qr, zl, zr): |
---|
| 315 | """Compute fluxes between volumes for the shallow water wave equation |
---|
| 316 | cast in terms of w = h+z using the 'central scheme' as described in |
---|
| 317 | |
---|
| 318 | Kurganov, Noelle, Petrova. 'Semidiscrete Central-Upwind Schemes For |
---|
| 319 | Hyperbolic Conservation Laws and Hamilton-Jacobi Equations'. |
---|
| 320 | Siam J. Sci. Comput. Vol. 23, No. 3, pp. 707-740. |
---|
| 321 | |
---|
| 322 | The implemented formula is given in equation (3.15) on page 714 |
---|
| 323 | |
---|
| 324 | Conserved quantities w, uh, vh are stored as elements 0, 1 and 2 |
---|
| 325 | in the numerical vectors ql an qr. |
---|
| 326 | |
---|
| 327 | Bed elevations zl and zr. |
---|
| 328 | """ |
---|
| 329 | |
---|
| 330 | from config import g, epsilon |
---|
| 331 | from math import sqrt |
---|
| 332 | from Numeric import array |
---|
| 333 | |
---|
| 334 | |
---|
| 335 | #Align momentums with x-axis |
---|
| 336 | q_left = rotate(ql, normal, direction = 1) |
---|
| 337 | q_right = rotate(qr, normal, direction = 1) |
---|
| 338 | |
---|
| 339 | z = (zl+zr)/2 #Take average of field values |
---|
| 340 | |
---|
| 341 | w_left = q_left[0] #w=h+z |
---|
| 342 | h_left = w_left-z |
---|
| 343 | uh_left = q_left[1] |
---|
| 344 | |
---|
| 345 | if h_left < epsilon: |
---|
| 346 | u_left = 0.0 #Could have been negative |
---|
| 347 | h_left = 0.0 |
---|
| 348 | else: |
---|
| 349 | u_left = uh_left/h_left |
---|
| 350 | |
---|
| 351 | |
---|
| 352 | w_right = q_right[0] #w=h+z |
---|
| 353 | h_right = w_right-z |
---|
| 354 | uh_right = q_right[1] |
---|
| 355 | |
---|
| 356 | |
---|
| 357 | if h_right < epsilon: |
---|
| 358 | u_right = 0.0 #Could have been negative |
---|
| 359 | h_right = 0.0 |
---|
| 360 | else: |
---|
| 361 | u_right = uh_right/h_right |
---|
| 362 | |
---|
| 363 | vh_left = q_left[2] |
---|
| 364 | vh_right = q_right[2] |
---|
| 365 | |
---|
| 366 | soundspeed_left = sqrt(g*h_left) |
---|
| 367 | soundspeed_right = sqrt(g*h_right) |
---|
| 368 | |
---|
| 369 | #Maximal wave speed |
---|
| 370 | s_max = max(u_left+soundspeed_left, u_right+soundspeed_right, 0) |
---|
| 371 | |
---|
| 372 | #Minimal wave speed |
---|
| 373 | s_min = min(u_left-soundspeed_left, u_right-soundspeed_right, 0) |
---|
| 374 | |
---|
| 375 | #Flux computation |
---|
| 376 | |
---|
| 377 | #FIXME(Ole): Why is it again that we don't |
---|
| 378 | #use uh_left and uh_right directly in the first entries? |
---|
| 379 | flux_left = array([u_left*h_left, |
---|
| 380 | u_left*uh_left + 0.5*g*h_left**2, |
---|
| 381 | u_left*vh_left]) |
---|
| 382 | flux_right = array([u_right*h_right, |
---|
| 383 | u_right*uh_right + 0.5*g*h_right**2, |
---|
| 384 | u_right*vh_right]) |
---|
| 385 | |
---|
| 386 | denom = s_max-s_min |
---|
| 387 | if denom == 0.0: |
---|
| 388 | edgeflux = array([0.0, 0.0, 0.0]) |
---|
| 389 | max_speed = 0.0 |
---|
| 390 | else: |
---|
| 391 | edgeflux = (s_max*flux_left - s_min*flux_right)/denom |
---|
| 392 | edgeflux += s_max*s_min*(q_right-q_left)/denom |
---|
| 393 | |
---|
| 394 | edgeflux = rotate(edgeflux, normal, direction=-1) |
---|
| 395 | max_speed = max(abs(s_max), abs(s_min)) |
---|
| 396 | |
---|
| 397 | return edgeflux, max_speed |
---|
| 398 | |
---|
| 399 | |
---|
| 400 | def erfcc(x): |
---|
| 401 | |
---|
| 402 | from math import fabs, exp |
---|
| 403 | |
---|
| 404 | z=fabs(x) |
---|
| 405 | t=1.0/(1.0+0.5*z) |
---|
| 406 | result=t*exp(-z*z-1.26551223+t*(1.00002368+t*(.37409196+ |
---|
| 407 | t*(.09678418+t*(-.18628806+t*(.27886807+t*(-1.13520398+ |
---|
| 408 | t*(1.48851587+t*(-.82215223+t*.17087277))))))))) |
---|
| 409 | if x < 0.0: |
---|
| 410 | result = 2.0-result |
---|
| 411 | |
---|
| 412 | return result |
---|
| 413 | |
---|
| 414 | def flux_function_kinetic(normal, ql, qr, zl, zr): |
---|
| 415 | """Compute fluxes between volumes for the shallow water wave equation |
---|
| 416 | cast in terms of w = h+z using the 'central scheme' as described in |
---|
| 417 | |
---|
| 418 | Zhang et. al., Advances in Water Resources, 26(6), 2003, 635-647. |
---|
| 419 | |
---|
| 420 | |
---|
| 421 | Conserved quantities w, uh, vh are stored as elements 0, 1 and 2 |
---|
| 422 | in the numerical vectors ql an qr. |
---|
| 423 | |
---|
| 424 | Bed elevations zl and zr. |
---|
| 425 | """ |
---|
| 426 | |
---|
| 427 | from config import g, epsilon |
---|
| 428 | from math import sqrt |
---|
| 429 | from Numeric import array |
---|
| 430 | |
---|
| 431 | #Align momentums with x-axis |
---|
| 432 | q_left = rotate(ql, normal, direction = 1) |
---|
| 433 | q_right = rotate(qr, normal, direction = 1) |
---|
| 434 | |
---|
| 435 | z = (zl+zr)/2 #Take average of field values |
---|
| 436 | |
---|
| 437 | w_left = q_left[0] #w=h+z |
---|
| 438 | h_left = w_left-z |
---|
| 439 | uh_left = q_left[1] |
---|
| 440 | |
---|
| 441 | if h_left < epsilon: |
---|
| 442 | u_left = 0.0 #Could have been negative |
---|
| 443 | h_left = 0.0 |
---|
| 444 | else: |
---|
| 445 | u_left = uh_left/h_left |
---|
| 446 | |
---|
| 447 | |
---|
| 448 | w_right = q_right[0] #w=h+z |
---|
| 449 | h_right = w_right-z |
---|
| 450 | uh_right = q_right[1] |
---|
| 451 | |
---|
| 452 | |
---|
| 453 | if h_right < epsilon: |
---|
| 454 | u_right = 0.0 #Could have been negative |
---|
| 455 | h_right = 0.0 |
---|
| 456 | else: |
---|
| 457 | u_right = uh_right/h_right |
---|
| 458 | |
---|
| 459 | vh_left = q_left[2] |
---|
| 460 | vh_right = q_right[2] |
---|
| 461 | |
---|
| 462 | soundspeed_left = sqrt(g*h_left) |
---|
| 463 | soundspeed_right = sqrt(g*h_right) |
---|
| 464 | |
---|
| 465 | #Maximal wave speed |
---|
| 466 | s_max = max(u_left+soundspeed_left, u_right+soundspeed_right, 0) |
---|
| 467 | |
---|
| 468 | #Minimal wave speed |
---|
| 469 | s_min = min(u_left-soundspeed_left, u_right-soundspeed_right, 0) |
---|
| 470 | |
---|
| 471 | #Flux computation |
---|
| 472 | |
---|
| 473 | F_left = 0.0 |
---|
| 474 | F_right = 0.0 |
---|
| 475 | from math import sqrt, pi, exp |
---|
| 476 | if h_left > 0.0: |
---|
| 477 | F_left = u_left/sqrt(g*h_left) |
---|
| 478 | if h_right > 0.0: |
---|
| 479 | F_right = u_right/sqrt(g*h_right) |
---|
| 480 | |
---|
| 481 | edgeflux = array([0.0, 0.0, 0.0]) |
---|
| 482 | |
---|
| 483 | edgeflux[0] = h_left*u_left/2.0*erfcc(-F_left) + \ |
---|
| 484 | h_left*sqrt(g*h_left)/2.0/sqrt(pi)*exp(-(F_left**2)) + \ |
---|
| 485 | h_right*u_right/2.0*erfcc(F_right) - \ |
---|
| 486 | h_right*sqrt(g*h_right)/2.0/sqrt(pi)*exp(-(F_right**2)) |
---|
| 487 | |
---|
| 488 | edgeflux[1] = (h_left*u_left**2 + g/2.0*h_left**2)/2.0*erfcc(-F_left) + \ |
---|
| 489 | u_left*h_left*sqrt(g*h_left)/2.0/sqrt(pi)*exp(-(F_left**2)) + \ |
---|
| 490 | (h_right*u_right**2 + g/2.0*h_right**2)/2.0*erfcc(F_right) - \ |
---|
| 491 | u_right*h_right*sqrt(g*h_right)/2.0/sqrt(pi)*exp(-(F_right**2)) |
---|
| 492 | |
---|
| 493 | edgeflux[2] = vh_left*u_left/2.0*erfcc(-F_left) + \ |
---|
| 494 | vh_left*sqrt(g*h_left)/2.0/sqrt(pi)*exp(-(F_left**2)) + \ |
---|
| 495 | vh_right*u_right/2.0*erfcc(F_right) - \ |
---|
| 496 | vh_right*sqrt(g*h_right)/2.0/sqrt(pi)*exp(-(F_right**2)) |
---|
| 497 | |
---|
| 498 | |
---|
| 499 | edgeflux = rotate(edgeflux, normal, direction=-1) |
---|
| 500 | max_speed = max(abs(s_max), abs(s_min)) |
---|
| 501 | |
---|
| 502 | return edgeflux, max_speed |
---|
| 503 | |
---|
| 504 | |
---|
| 505 | flux_function = flux_function_kinetic |
---|
| 506 | |
---|
| 507 | def compute_fluxes(domain): |
---|
| 508 | """Compute all fluxes and the timestep suitable for all volumes |
---|
| 509 | in domain. |
---|
| 510 | |
---|
| 511 | Compute total flux for each conserved quantity using "flux_function" |
---|
| 512 | |
---|
| 513 | Fluxes across each edge are scaled by edgelengths and summed up |
---|
| 514 | Resulting flux is then scaled by area and stored in |
---|
| 515 | explicit_update for each of the three conserved quantities |
---|
| 516 | stage, xmomentum and ymomentum |
---|
| 517 | |
---|
| 518 | The maximal allowable speed computed by the flux_function for each volume |
---|
| 519 | is converted to a timestep that must not be exceeded. The minimum of |
---|
| 520 | those is computed as the next overall timestep. |
---|
| 521 | |
---|
| 522 | Post conditions: |
---|
| 523 | domain.explicit_update is reset to computed flux values |
---|
| 524 | domain.timestep is set to the largest step satisfying all volumes. |
---|
| 525 | """ |
---|
| 526 | |
---|
| 527 | import sys |
---|
| 528 | from Numeric import zeros, Float |
---|
| 529 | |
---|
| 530 | N = domain.number_of_elements |
---|
| 531 | |
---|
| 532 | |
---|
| 533 | #Shortcuts |
---|
| 534 | Stage = domain.quantities['stage'] |
---|
| 535 | Xmom = domain.quantities['xmomentum'] |
---|
| 536 | Ymom = domain.quantities['ymomentum'] |
---|
| 537 | Bed = domain.quantities['elevation'] |
---|
| 538 | |
---|
| 539 | #Arrays |
---|
| 540 | stage = Stage.edge_values |
---|
| 541 | xmom = Xmom.edge_values |
---|
| 542 | ymom = Ymom.edge_values |
---|
| 543 | bed = Bed.edge_values |
---|
| 544 | |
---|
| 545 | stage_bdry = Stage.boundary_values |
---|
| 546 | xmom_bdry = Xmom.boundary_values |
---|
| 547 | ymom_bdry = Ymom.boundary_values |
---|
| 548 | |
---|
| 549 | flux = zeros(3, Float) #Work array for summing up fluxes |
---|
| 550 | |
---|
| 551 | |
---|
| 552 | #Loop |
---|
| 553 | timestep = float(sys.maxint) |
---|
| 554 | for k in range(N): |
---|
| 555 | |
---|
| 556 | flux[:] = 0. #Reset work array |
---|
| 557 | for i in range(3): |
---|
| 558 | #Quantities inside volume facing neighbour i |
---|
| 559 | ql = [stage[k, i], xmom[k, i], ymom[k, i]] |
---|
| 560 | zl = bed[k, i] |
---|
| 561 | |
---|
| 562 | #Quantities at neighbour on nearest face |
---|
| 563 | n = domain.neighbours[k,i] |
---|
| 564 | if n < 0: |
---|
| 565 | m = -n-1 #Convert negative flag to index |
---|
| 566 | qr = [stage_bdry[m], xmom_bdry[m], ymom_bdry[m]] |
---|
| 567 | zr = zl #Extend bed elevation to boundary |
---|
| 568 | else: |
---|
| 569 | m = domain.neighbour_edges[k,i] |
---|
| 570 | qr = [stage[n, m], xmom[n, m], ymom[n, m]] |
---|
| 571 | zr = bed[n, m] |
---|
| 572 | |
---|
| 573 | |
---|
| 574 | #Outward pointing normal vector |
---|
| 575 | normal = domain.normals[k, 2*i:2*i+2] |
---|
| 576 | |
---|
| 577 | #Flux computation using provided function |
---|
| 578 | edgeflux, max_speed = flux_function(normal, ql, qr, zl, zr) |
---|
| 579 | flux -= edgeflux * domain.edgelengths[k,i] |
---|
| 580 | |
---|
| 581 | #Update optimal_timestep |
---|
| 582 | try: |
---|
| 583 | timestep = min(timestep, 0.5*domain.radii[k]/max_speed) |
---|
| 584 | except ZeroDivisionError: |
---|
| 585 | pass |
---|
| 586 | |
---|
| 587 | #Normalise by area and store for when all conserved |
---|
| 588 | #quantities get updated |
---|
| 589 | flux /= domain.areas[k] |
---|
| 590 | Stage.explicit_update[k] = flux[0] |
---|
| 591 | Xmom.explicit_update[k] = flux[1] |
---|
| 592 | Ymom.explicit_update[k] = flux[2] |
---|
| 593 | |
---|
| 594 | |
---|
| 595 | domain.timestep = timestep |
---|
| 596 | |
---|
| 597 | #MH090605 The following method belongs to the shallow_water domain class |
---|
| 598 | #see comments in the corresponding method in shallow_water_ext.c |
---|
| 599 | def extrapolate_second_order_sw_c(domain): |
---|
| 600 | """Wrapper calling C version of extrapolate_second_order_sw |
---|
| 601 | """ |
---|
| 602 | import sys |
---|
| 603 | from Numeric import zeros, Float |
---|
| 604 | |
---|
| 605 | N = domain.number_of_elements |
---|
| 606 | |
---|
| 607 | #Shortcuts |
---|
| 608 | Stage = domain.quantities['stage'] |
---|
| 609 | Xmom = domain.quantities['xmomentum'] |
---|
| 610 | Ymom = domain.quantities['ymomentum'] |
---|
| 611 | from shallow_water_ext import extrapolate_second_order_sw |
---|
| 612 | extrapolate_second_order_sw(domain,domain.surrogate_neighbours, |
---|
| 613 | domain.number_of_boundaries, |
---|
| 614 | domain.centroid_coordinates, |
---|
| 615 | Stage.centroid_values, |
---|
| 616 | Xmom.centroid_values, |
---|
| 617 | Ymom.centroid_values, |
---|
| 618 | domain.vertex_coordinates, |
---|
| 619 | Stage.vertex_values, |
---|
| 620 | Xmom.vertex_values, |
---|
| 621 | Ymom.vertex_values) |
---|
| 622 | |
---|
| 623 | def compute_fluxes_c(domain): |
---|
| 624 | """Wrapper calling C version of compute fluxes |
---|
| 625 | """ |
---|
| 626 | |
---|
| 627 | import sys |
---|
| 628 | from Numeric import zeros, Float |
---|
| 629 | |
---|
| 630 | N = domain.number_of_elements |
---|
| 631 | |
---|
| 632 | #Shortcuts |
---|
| 633 | Stage = domain.quantities['stage'] |
---|
| 634 | Xmom = domain.quantities['xmomentum'] |
---|
| 635 | Ymom = domain.quantities['ymomentum'] |
---|
| 636 | Bed = domain.quantities['elevation'] |
---|
| 637 | |
---|
| 638 | timestep = float(sys.maxint) |
---|
| 639 | from shallow_water_ext import compute_fluxes |
---|
| 640 | domain.timestep = compute_fluxes(timestep, domain.epsilon, domain.g, |
---|
| 641 | domain.neighbours, |
---|
| 642 | domain.neighbour_edges, |
---|
| 643 | domain.normals, |
---|
| 644 | domain.edgelengths, |
---|
| 645 | domain.radii, |
---|
| 646 | domain.areas, |
---|
| 647 | Stage.edge_values, |
---|
| 648 | Xmom.edge_values, |
---|
| 649 | Ymom.edge_values, |
---|
| 650 | Bed.edge_values, |
---|
| 651 | Stage.boundary_values, |
---|
| 652 | Xmom.boundary_values, |
---|
| 653 | Ymom.boundary_values, |
---|
| 654 | Stage.explicit_update, |
---|
| 655 | Xmom.explicit_update, |
---|
| 656 | Ymom.explicit_update, |
---|
| 657 | domain.already_computed_flux) |
---|
| 658 | |
---|
| 659 | |
---|
| 660 | #################################### |
---|
| 661 | # Module functions for gradient limiting (distribute_to_vertices_and_edges) |
---|
| 662 | |
---|
| 663 | def distribute_to_vertices_and_edges(domain): |
---|
| 664 | """Distribution from centroids to vertices specific to the |
---|
| 665 | shallow water wave |
---|
| 666 | equation. |
---|
| 667 | |
---|
| 668 | It will ensure that h (w-z) is always non-negative even in the |
---|
| 669 | presence of steep bed-slopes by taking a weighted average between shallow |
---|
| 670 | and deep cases. |
---|
| 671 | |
---|
| 672 | In addition, all conserved quantities get distributed as per either a |
---|
| 673 | constant (order==1) or a piecewise linear function (order==2). |
---|
| 674 | |
---|
| 675 | FIXME: more explanation about removal of artificial variability etc |
---|
| 676 | |
---|
| 677 | Precondition: |
---|
| 678 | All quantities defined at centroids and bed elevation defined at |
---|
| 679 | vertices. |
---|
| 680 | |
---|
| 681 | Postcondition |
---|
| 682 | Conserved quantities defined at vertices |
---|
| 683 | |
---|
| 684 | """ |
---|
| 685 | |
---|
| 686 | from config import optimised_gradient_limiter |
---|
| 687 | |
---|
| 688 | #Remove very thin layers of water |
---|
| 689 | protect_against_infinitesimal_and_negative_heights(domain) |
---|
| 690 | |
---|
| 691 | #Extrapolate all conserved quantities |
---|
| 692 | if optimised_gradient_limiter: |
---|
| 693 | #MH090605 if second order, |
---|
| 694 | #perform the extrapolation and limiting on |
---|
| 695 | #all of the conserved quantitie |
---|
| 696 | |
---|
| 697 | if (domain.order == 1): |
---|
| 698 | for name in domain.conserved_quantities: |
---|
| 699 | Q = domain.quantities[name] |
---|
| 700 | Q.extrapolate_first_order() |
---|
| 701 | elif domain.order == 2: |
---|
| 702 | domain.extrapolate_second_order_sw() |
---|
| 703 | else: |
---|
| 704 | raise 'Unknown order' |
---|
| 705 | else: |
---|
| 706 | #old code: |
---|
| 707 | for name in domain.conserved_quantities: |
---|
| 708 | Q = domain.quantities[name] |
---|
| 709 | if domain.order == 1: |
---|
| 710 | Q.extrapolate_first_order() |
---|
| 711 | elif domain.order == 2: |
---|
| 712 | Q.extrapolate_second_order() |
---|
| 713 | Q.limit() |
---|
| 714 | else: |
---|
| 715 | raise 'Unknown order' |
---|
| 716 | |
---|
| 717 | |
---|
| 718 | #Take bed elevation into account when water heights are small |
---|
| 719 | balance_deep_and_shallow(domain) |
---|
| 720 | |
---|
| 721 | #Compute edge values by interpolation |
---|
| 722 | for name in domain.conserved_quantities: |
---|
| 723 | Q = domain.quantities[name] |
---|
| 724 | Q.interpolate_from_vertices_to_edges() |
---|
| 725 | |
---|
| 726 | |
---|
| 727 | def protect_against_infinitesimal_and_negative_heights(domain): |
---|
| 728 | """Protect against infinitesimal heights and associated high velocities |
---|
| 729 | """ |
---|
| 730 | |
---|
| 731 | #Shortcuts |
---|
| 732 | wc = domain.quantities['stage'].centroid_values |
---|
| 733 | zc = domain.quantities['elevation'].centroid_values |
---|
| 734 | xmomc = domain.quantities['xmomentum'].centroid_values |
---|
| 735 | ymomc = domain.quantities['ymomentum'].centroid_values |
---|
| 736 | hc = wc - zc #Water depths at centroids |
---|
| 737 | |
---|
| 738 | #Update |
---|
| 739 | for k in range(domain.number_of_elements): |
---|
| 740 | |
---|
| 741 | if hc[k] < domain.minimum_allowed_height: |
---|
| 742 | #Control stage |
---|
| 743 | if hc[k] < domain.epsilon: |
---|
| 744 | wc[k] = zc[k] # Contain 'lost mass' error |
---|
| 745 | |
---|
| 746 | #Control momentum |
---|
| 747 | xmomc[k] = ymomc[k] = 0.0 |
---|
| 748 | |
---|
| 749 | |
---|
| 750 | def protect_against_infinitesimal_and_negative_heights_c(domain): |
---|
| 751 | """Protect against infinitesimal heights and associated high velocities |
---|
| 752 | """ |
---|
| 753 | |
---|
| 754 | #Shortcuts |
---|
| 755 | wc = domain.quantities['stage'].centroid_values |
---|
| 756 | zc = domain.quantities['elevation'].centroid_values |
---|
| 757 | xmomc = domain.quantities['xmomentum'].centroid_values |
---|
| 758 | ymomc = domain.quantities['ymomentum'].centroid_values |
---|
| 759 | |
---|
| 760 | from shallow_water_ext import protect |
---|
| 761 | |
---|
| 762 | protect(domain.minimum_allowed_height, domain.epsilon, |
---|
| 763 | wc, zc, xmomc, ymomc) |
---|
| 764 | |
---|
| 765 | |
---|
| 766 | |
---|
| 767 | def h_limiter(domain): |
---|
| 768 | """Limit slopes for each volume to eliminate artificial variance |
---|
| 769 | introduced by e.g. second order extrapolator |
---|
| 770 | |
---|
| 771 | limit on h = w-z |
---|
| 772 | |
---|
| 773 | This limiter depends on two quantities (w,z) so it resides within |
---|
| 774 | this module rather than within quantity.py |
---|
| 775 | """ |
---|
| 776 | |
---|
| 777 | from Numeric import zeros, Float |
---|
| 778 | |
---|
| 779 | N = domain.number_of_elements |
---|
| 780 | beta_h = domain.beta_h |
---|
| 781 | |
---|
| 782 | #Shortcuts |
---|
| 783 | wc = domain.quantities['stage'].centroid_values |
---|
| 784 | zc = domain.quantities['elevation'].centroid_values |
---|
| 785 | hc = wc - zc |
---|
| 786 | |
---|
| 787 | wv = domain.quantities['stage'].vertex_values |
---|
| 788 | zv = domain.quantities['elevation'].vertex_values |
---|
| 789 | hv = wv-zv |
---|
| 790 | |
---|
| 791 | hvbar = zeros(hv.shape, Float) #h-limited values |
---|
| 792 | |
---|
| 793 | #Find min and max of this and neighbour's centroid values |
---|
| 794 | hmax = zeros(hc.shape, Float) |
---|
| 795 | hmin = zeros(hc.shape, Float) |
---|
| 796 | |
---|
| 797 | for k in range(N): |
---|
| 798 | hmax[k] = hmin[k] = hc[k] |
---|
| 799 | for i in range(3): |
---|
| 800 | n = domain.neighbours[k,i] |
---|
| 801 | if n >= 0: |
---|
| 802 | hn = hc[n] #Neighbour's centroid value |
---|
| 803 | |
---|
| 804 | hmin[k] = min(hmin[k], hn) |
---|
| 805 | hmax[k] = max(hmax[k], hn) |
---|
| 806 | |
---|
| 807 | |
---|
| 808 | #Diffences between centroids and maxima/minima |
---|
| 809 | dhmax = hmax - hc |
---|
| 810 | dhmin = hmin - hc |
---|
| 811 | |
---|
| 812 | #Deltas between vertex and centroid values |
---|
| 813 | dh = zeros(hv.shape, Float) |
---|
| 814 | for i in range(3): |
---|
| 815 | dh[:,i] = hv[:,i] - hc |
---|
| 816 | |
---|
| 817 | #Phi limiter |
---|
| 818 | for k in range(N): |
---|
| 819 | |
---|
| 820 | #Find the gradient limiter (phi) across vertices |
---|
| 821 | phi = 1.0 |
---|
| 822 | for i in range(3): |
---|
| 823 | r = 1.0 |
---|
| 824 | if (dh[k,i] > 0): r = dhmax[k]/dh[k,i] |
---|
| 825 | if (dh[k,i] < 0): r = dhmin[k]/dh[k,i] |
---|
| 826 | |
---|
| 827 | phi = min( min(r*beta_h, 1), phi ) |
---|
| 828 | |
---|
| 829 | #Then update using phi limiter |
---|
| 830 | for i in range(3): |
---|
| 831 | hvbar[k,i] = hc[k] + phi*dh[k,i] |
---|
| 832 | |
---|
| 833 | return hvbar |
---|
| 834 | |
---|
| 835 | |
---|
| 836 | |
---|
| 837 | def h_limiter_c(domain): |
---|
| 838 | """Limit slopes for each volume to eliminate artificial variance |
---|
| 839 | introduced by e.g. second order extrapolator |
---|
| 840 | |
---|
| 841 | limit on h = w-z |
---|
| 842 | |
---|
| 843 | This limiter depends on two quantities (w,z) so it resides within |
---|
| 844 | this module rather than within quantity.py |
---|
| 845 | |
---|
| 846 | Wrapper for c-extension |
---|
| 847 | """ |
---|
| 848 | |
---|
| 849 | from Numeric import zeros, Float |
---|
| 850 | |
---|
| 851 | N = domain.number_of_elements |
---|
| 852 | beta_h = domain.beta_h |
---|
| 853 | |
---|
| 854 | #Shortcuts |
---|
| 855 | wc = domain.quantities['stage'].centroid_values |
---|
| 856 | zc = domain.quantities['elevation'].centroid_values |
---|
| 857 | hc = wc - zc |
---|
| 858 | |
---|
| 859 | wv = domain.quantities['stage'].vertex_values |
---|
| 860 | zv = domain.quantities['elevation'].vertex_values |
---|
| 861 | hv = wv - zv |
---|
| 862 | |
---|
| 863 | #Call C-extension |
---|
| 864 | from shallow_water_ext import h_limiter_sw as h_limiter |
---|
| 865 | hvbar = h_limiter(domain, hc, hv) |
---|
| 866 | |
---|
| 867 | return hvbar |
---|
| 868 | |
---|
| 869 | |
---|
| 870 | def balance_deep_and_shallow(domain): |
---|
| 871 | """Compute linear combination between stage as computed by |
---|
| 872 | gradient-limiters limiting using w, and stage computed by |
---|
| 873 | gradient-limiters limiting using h (h-limiter). |
---|
| 874 | The former takes precedence when heights are large compared to the |
---|
| 875 | bed slope while the latter takes precedence when heights are |
---|
| 876 | relatively small. Anything in between is computed as a balanced |
---|
| 877 | linear combination in order to avoid numerical disturbances which |
---|
| 878 | would otherwise appear as a result of hard switching between |
---|
| 879 | modes. |
---|
| 880 | |
---|
| 881 | The h-limiter is always applied irrespective of the order. |
---|
| 882 | """ |
---|
| 883 | |
---|
| 884 | #Shortcuts |
---|
| 885 | wc = domain.quantities['stage'].centroid_values |
---|
| 886 | zc = domain.quantities['elevation'].centroid_values |
---|
| 887 | hc = wc - zc |
---|
| 888 | |
---|
| 889 | wv = domain.quantities['stage'].vertex_values |
---|
| 890 | zv = domain.quantities['elevation'].vertex_values |
---|
| 891 | hv = wv-zv |
---|
| 892 | |
---|
| 893 | #Limit h |
---|
| 894 | hvbar = h_limiter(domain) |
---|
| 895 | |
---|
| 896 | for k in range(domain.number_of_elements): |
---|
| 897 | #Compute maximal variation in bed elevation |
---|
| 898 | # This quantitiy is |
---|
| 899 | # dz = max_i abs(z_i - z_c) |
---|
| 900 | # and it is independent of dimension |
---|
| 901 | # In the 1d case zc = (z0+z1)/2 |
---|
| 902 | # In the 2d case zc = (z0+z1+z2)/3 |
---|
| 903 | |
---|
| 904 | dz = max(abs(zv[k,0]-zc[k]), |
---|
| 905 | abs(zv[k,1]-zc[k]), |
---|
| 906 | abs(zv[k,2]-zc[k])) |
---|
| 907 | |
---|
| 908 | |
---|
| 909 | hmin = min( hv[k,:] ) |
---|
| 910 | |
---|
| 911 | #Create alpha in [0,1], where alpha==0 means using the h-limited |
---|
| 912 | #stage and alpha==1 means using the w-limited stage as |
---|
| 913 | #computed by the gradient limiter (both 1st or 2nd order) |
---|
| 914 | |
---|
| 915 | #If hmin > dz/2 then alpha = 1 and the bed will have no effect |
---|
| 916 | #If hmin < 0 then alpha = 0 reverting to constant height above bed. |
---|
| 917 | |
---|
| 918 | if dz > 0.0: |
---|
| 919 | alpha = max( min( 2*hmin/dz, 1.0), 0.0 ) |
---|
| 920 | else: |
---|
| 921 | #Flat bed |
---|
| 922 | alpha = 1.0 |
---|
| 923 | |
---|
| 924 | #Let |
---|
| 925 | # |
---|
| 926 | # wvi be the w-limited stage (wvi = zvi + hvi) |
---|
| 927 | # wvi- be the h-limited state (wvi- = zvi + hvi-) |
---|
| 928 | # |
---|
| 929 | # |
---|
| 930 | #where i=0,1,2 denotes the vertex ids |
---|
| 931 | # |
---|
| 932 | #Weighted balance between w-limited and h-limited stage is |
---|
| 933 | # |
---|
| 934 | # wvi := (1-alpha)*(zvi+hvi-) + alpha*(zvi+hvi) |
---|
| 935 | # |
---|
| 936 | #It follows that the updated wvi is |
---|
| 937 | # wvi := zvi + (1-alpha)*hvi- + alpha*hvi |
---|
| 938 | # |
---|
| 939 | # Momentum is balanced between constant and limited |
---|
| 940 | |
---|
| 941 | |
---|
| 942 | #for i in range(3): |
---|
| 943 | # wv[k,i] = zv[k,i] + hvbar[k,i] |
---|
| 944 | |
---|
| 945 | #return |
---|
| 946 | |
---|
| 947 | if alpha < 1: |
---|
| 948 | |
---|
| 949 | for i in range(3): |
---|
| 950 | wv[k,i] = zv[k,i] + (1-alpha)*hvbar[k,i] + alpha*hv[k,i] |
---|
| 951 | |
---|
| 952 | #Momentums at centroids |
---|
| 953 | xmomc = domain.quantities['xmomentum'].centroid_values |
---|
| 954 | ymomc = domain.quantities['ymomentum'].centroid_values |
---|
| 955 | |
---|
| 956 | #Momentums at vertices |
---|
| 957 | xmomv = domain.quantities['xmomentum'].vertex_values |
---|
| 958 | ymomv = domain.quantities['ymomentum'].vertex_values |
---|
| 959 | |
---|
| 960 | # Update momentum as a linear combination of |
---|
| 961 | # xmomc and ymomc (shallow) and momentum |
---|
| 962 | # from extrapolator xmomv and ymomv (deep). |
---|
| 963 | xmomv[k,:] = (1-alpha)*xmomc[k] + alpha*xmomv[k,:] |
---|
| 964 | ymomv[k,:] = (1-alpha)*ymomc[k] + alpha*ymomv[k,:] |
---|
| 965 | |
---|
| 966 | |
---|
| 967 | def balance_deep_and_shallow_c(domain): |
---|
| 968 | """Wrapper for C implementation |
---|
| 969 | """ |
---|
| 970 | |
---|
| 971 | #Shortcuts |
---|
| 972 | wc = domain.quantities['stage'].centroid_values |
---|
| 973 | zc = domain.quantities['elevation'].centroid_values |
---|
| 974 | hc = wc - zc |
---|
| 975 | |
---|
| 976 | wv = domain.quantities['stage'].vertex_values |
---|
| 977 | zv = domain.quantities['elevation'].vertex_values |
---|
| 978 | hv = wv - zv |
---|
| 979 | |
---|
| 980 | #Momentums at centroids |
---|
| 981 | xmomc = domain.quantities['xmomentum'].centroid_values |
---|
| 982 | ymomc = domain.quantities['ymomentum'].centroid_values |
---|
| 983 | |
---|
| 984 | #Momentums at vertices |
---|
| 985 | xmomv = domain.quantities['xmomentum'].vertex_values |
---|
| 986 | ymomv = domain.quantities['ymomentum'].vertex_values |
---|
| 987 | |
---|
| 988 | #Limit h |
---|
| 989 | hvbar = h_limiter(domain) |
---|
| 990 | |
---|
| 991 | #This is how one would make a first order h_limited value |
---|
| 992 | #as in the old balancer (pre 17 Feb 2005): |
---|
| 993 | #from Numeric import zeros, Float |
---|
| 994 | #hvbar = zeros( (len(hc), 3), Float) |
---|
| 995 | #for i in range(3): |
---|
| 996 | # hvbar[:,i] = hc[:] |
---|
| 997 | |
---|
| 998 | from shallow_water_ext import balance_deep_and_shallow |
---|
| 999 | balance_deep_and_shallow(wc, zc, hc, wv, zv, hv, hvbar, |
---|
| 1000 | xmomc, ymomc, xmomv, ymomv) |
---|
| 1001 | |
---|
| 1002 | |
---|
| 1003 | |
---|
| 1004 | |
---|
| 1005 | ############################################### |
---|
| 1006 | #Boundaries - specific to the shallow water wave equation |
---|
| 1007 | class Reflective_boundary(Boundary): |
---|
| 1008 | """Reflective boundary returns same conserved quantities as |
---|
| 1009 | those present in its neighbour volume but reflected. |
---|
| 1010 | |
---|
| 1011 | This class is specific to the shallow water equation as it |
---|
| 1012 | works with the momentum quantities assumed to be the second |
---|
| 1013 | and third conserved quantities. |
---|
| 1014 | """ |
---|
| 1015 | |
---|
| 1016 | def __init__(self, domain = None): |
---|
| 1017 | Boundary.__init__(self) |
---|
| 1018 | |
---|
| 1019 | if domain is None: |
---|
| 1020 | msg = 'Domain must be specified for reflective boundary' |
---|
| 1021 | raise msg |
---|
| 1022 | |
---|
| 1023 | #Handy shorthands |
---|
| 1024 | self.stage = domain.quantities['stage'].edge_values |
---|
| 1025 | self.xmom = domain.quantities['xmomentum'].edge_values |
---|
| 1026 | self.ymom = domain.quantities['ymomentum'].edge_values |
---|
| 1027 | self.normals = domain.normals |
---|
| 1028 | |
---|
| 1029 | from Numeric import zeros, Float |
---|
| 1030 | self.conserved_quantities = zeros(3, Float) |
---|
| 1031 | |
---|
| 1032 | def __repr__(self): |
---|
| 1033 | return 'Reflective_boundary' |
---|
| 1034 | |
---|
| 1035 | |
---|
| 1036 | def evaluate(self, vol_id, edge_id): |
---|
| 1037 | """Reflective boundaries reverses the outward momentum |
---|
| 1038 | of the volume they serve. |
---|
| 1039 | """ |
---|
| 1040 | |
---|
| 1041 | q = self.conserved_quantities |
---|
| 1042 | q[0] = self.stage[vol_id, edge_id] |
---|
| 1043 | q[1] = self.xmom[vol_id, edge_id] |
---|
| 1044 | q[2] = self.ymom[vol_id, edge_id] |
---|
| 1045 | |
---|
| 1046 | normal = self.normals[vol_id, 2*edge_id:2*edge_id+2] |
---|
| 1047 | |
---|
| 1048 | |
---|
| 1049 | r = rotate(q, normal, direction = 1) |
---|
| 1050 | r[1] = -r[1] |
---|
| 1051 | q = rotate(r, normal, direction = -1) |
---|
| 1052 | |
---|
| 1053 | return q |
---|
| 1054 | |
---|
| 1055 | |
---|
| 1056 | |
---|
| 1057 | class Transmissive_Momentum_Set_Stage_boundary(Boundary): |
---|
| 1058 | """Returns same momentum conserved quantities as |
---|
| 1059 | those present in its neighbour volume. Sets stage |
---|
| 1060 | |
---|
| 1061 | Underlying domain must be specified when boundary is instantiated |
---|
| 1062 | """ |
---|
| 1063 | |
---|
| 1064 | def __init__(self, domain = None, function=None): |
---|
| 1065 | Boundary.__init__(self) |
---|
| 1066 | |
---|
| 1067 | if domain is None: |
---|
| 1068 | msg = 'Domain must be specified for this type boundary' |
---|
| 1069 | raise msg |
---|
| 1070 | |
---|
| 1071 | if function is None: |
---|
| 1072 | msg = 'Function must be specified for this type boundary' |
---|
| 1073 | raise msg |
---|
| 1074 | |
---|
| 1075 | self.domain = domain |
---|
| 1076 | self.function = function |
---|
| 1077 | |
---|
| 1078 | def __repr__(self): |
---|
| 1079 | return 'Transmissive_Momentum_Set_Stage_boundary(%s)' %self.domain |
---|
| 1080 | |
---|
| 1081 | def evaluate(self, vol_id, edge_id): |
---|
| 1082 | """Transmissive Momentum Set Stage boundaries return the edge momentum |
---|
| 1083 | values of the volume they serve. |
---|
| 1084 | """ |
---|
| 1085 | |
---|
| 1086 | q = self.domain.get_conserved_quantities(vol_id, edge = edge_id) |
---|
| 1087 | value = self.function(self.domain.time) |
---|
| 1088 | q[0] = value[0] |
---|
| 1089 | return q |
---|
| 1090 | |
---|
| 1091 | |
---|
| 1092 | #FIXME: Consider this (taken from File_boundary) to allow |
---|
| 1093 | #spatial variation |
---|
| 1094 | #if vol_id is not None and edge_id is not None: |
---|
| 1095 | # i = self.boundary_indices[ vol_id, edge_id ] |
---|
| 1096 | # return self.F(t, point_id = i) |
---|
| 1097 | #else: |
---|
| 1098 | # return self.F(t) |
---|
| 1099 | |
---|
| 1100 | |
---|
| 1101 | |
---|
| 1102 | class Dirichlet_Discharge_boundary(Boundary): |
---|
| 1103 | """ |
---|
| 1104 | Sets stage (stage0) |
---|
| 1105 | Sets momentum (wh0) in the inward normal direction. |
---|
| 1106 | |
---|
| 1107 | Underlying domain must be specified when boundary is instantiated |
---|
| 1108 | """ |
---|
| 1109 | |
---|
| 1110 | def __init__(self, domain = None, stage0=None, wh0=None): |
---|
| 1111 | Boundary.__init__(self) |
---|
| 1112 | |
---|
| 1113 | if domain is None: |
---|
| 1114 | msg = 'Domain must be specified for this type boundary' |
---|
| 1115 | raise msg |
---|
| 1116 | |
---|
| 1117 | if stage0 is None: |
---|
| 1118 | raise 'set stage' |
---|
| 1119 | |
---|
| 1120 | if wh0 is None: |
---|
| 1121 | wh0 = 0.0 |
---|
| 1122 | |
---|
| 1123 | self.domain = domain |
---|
| 1124 | self.stage0 = stage0 |
---|
| 1125 | self.wh0 = wh0 |
---|
| 1126 | |
---|
| 1127 | def __repr__(self): |
---|
| 1128 | return 'Dirichlet_Discharge_boundary(%s)' %self.domain |
---|
| 1129 | |
---|
| 1130 | def evaluate(self, vol_id, edge_id): |
---|
| 1131 | """Set discharge in the (inward) normal direction |
---|
| 1132 | """ |
---|
| 1133 | |
---|
| 1134 | normal = self.domain.get_normal(vol_id,edge_id) |
---|
| 1135 | q = [self.stage0, -self.wh0*normal[0], -self.wh0*normal[1]] |
---|
| 1136 | return q |
---|
| 1137 | |
---|
| 1138 | |
---|
| 1139 | #FIXME: Consider this (taken from File_boundary) to allow |
---|
| 1140 | #spatial variation |
---|
| 1141 | #if vol_id is not None and edge_id is not None: |
---|
| 1142 | # i = self.boundary_indices[ vol_id, edge_id ] |
---|
| 1143 | # return self.F(t, point_id = i) |
---|
| 1144 | #else: |
---|
| 1145 | # return self.F(t) |
---|
| 1146 | |
---|
| 1147 | |
---|
| 1148 | |
---|
| 1149 | #class Spatio_temporal_boundary(Boundary): |
---|
| 1150 | # """The spatio-temporal boundary, reads values for the conserved |
---|
| 1151 | # quantities from an sww NetCDF file, and returns interpolated values |
---|
| 1152 | # at the midpoints of each associated boundaty segment. |
---|
| 1153 | # Time dependency is interpolated linearly as in util.File_function.# |
---|
| 1154 | # |
---|
| 1155 | # Example: |
---|
| 1156 | # Bf = Spatio_temporal_boundary('source_file.sww', domain) |
---|
| 1157 | # |
---|
| 1158 | # """ |
---|
| 1159 | Spatio_temporal_boundary = File_boundary |
---|
| 1160 | |
---|
| 1161 | |
---|
| 1162 | |
---|
| 1163 | |
---|
| 1164 | ######################### |
---|
| 1165 | #Standard forcing terms: |
---|
| 1166 | # |
---|
| 1167 | def gravity(domain): |
---|
| 1168 | """Apply gravitational pull in the presence of bed slope |
---|
| 1169 | """ |
---|
| 1170 | |
---|
| 1171 | from util import gradient |
---|
| 1172 | from Numeric import zeros, Float, array, sum |
---|
| 1173 | |
---|
| 1174 | xmom = domain.quantities['xmomentum'].explicit_update |
---|
| 1175 | ymom = domain.quantities['ymomentum'].explicit_update |
---|
| 1176 | |
---|
| 1177 | Stage = domain.quantities['stage'] |
---|
| 1178 | Elevation = domain.quantities['elevation'] |
---|
| 1179 | h = Stage.edge_values - Elevation.edge_values |
---|
| 1180 | v = Elevation.vertex_values |
---|
| 1181 | |
---|
| 1182 | x = domain.get_vertex_coordinates() |
---|
| 1183 | g = domain.g |
---|
| 1184 | |
---|
| 1185 | for k in range(domain.number_of_elements): |
---|
| 1186 | avg_h = sum( h[k,:] )/3 |
---|
| 1187 | |
---|
| 1188 | #Compute bed slope |
---|
| 1189 | x0, y0, x1, y1, x2, y2 = x[k,:] |
---|
| 1190 | z0, z1, z2 = v[k,:] |
---|
| 1191 | |
---|
| 1192 | zx, zy = gradient(x0, y0, x1, y1, x2, y2, z0, z1, z2) |
---|
| 1193 | |
---|
| 1194 | #Update momentum |
---|
| 1195 | xmom[k] += -g*zx*avg_h |
---|
| 1196 | ymom[k] += -g*zy*avg_h |
---|
| 1197 | |
---|
| 1198 | |
---|
| 1199 | def gravity_c(domain): |
---|
| 1200 | """Wrapper calling C version |
---|
| 1201 | """ |
---|
| 1202 | |
---|
| 1203 | xmom = domain.quantities['xmomentum'].explicit_update |
---|
| 1204 | ymom = domain.quantities['ymomentum'].explicit_update |
---|
| 1205 | |
---|
| 1206 | Stage = domain.quantities['stage'] |
---|
| 1207 | Elevation = domain.quantities['elevation'] |
---|
| 1208 | h = Stage.edge_values - Elevation.edge_values |
---|
| 1209 | v = Elevation.vertex_values |
---|
| 1210 | |
---|
| 1211 | x = domain.get_vertex_coordinates() |
---|
| 1212 | g = domain.g |
---|
| 1213 | |
---|
| 1214 | |
---|
| 1215 | from shallow_water_ext import gravity |
---|
| 1216 | gravity(g, h, v, x, xmom, ymom) |
---|
| 1217 | |
---|
| 1218 | |
---|
| 1219 | def manning_friction(domain): |
---|
| 1220 | """Apply (Manning) friction to water momentum |
---|
| 1221 | """ |
---|
| 1222 | |
---|
| 1223 | from math import sqrt |
---|
| 1224 | |
---|
| 1225 | w = domain.quantities['stage'].centroid_values |
---|
| 1226 | z = domain.quantities['elevation'].centroid_values |
---|
| 1227 | h = w-z |
---|
| 1228 | |
---|
| 1229 | uh = domain.quantities['xmomentum'].centroid_values |
---|
| 1230 | vh = domain.quantities['ymomentum'].centroid_values |
---|
| 1231 | eta = domain.quantities['friction'].centroid_values |
---|
| 1232 | |
---|
| 1233 | xmom_update = domain.quantities['xmomentum'].semi_implicit_update |
---|
| 1234 | ymom_update = domain.quantities['ymomentum'].semi_implicit_update |
---|
| 1235 | |
---|
| 1236 | N = domain.number_of_elements |
---|
| 1237 | eps = domain.minimum_allowed_height |
---|
| 1238 | g = domain.g |
---|
| 1239 | |
---|
| 1240 | for k in range(N): |
---|
| 1241 | if eta[k] >= eps: |
---|
| 1242 | if h[k] >= eps: |
---|
| 1243 | S = -g * eta[k]**2 * sqrt((uh[k]**2 + vh[k]**2)) |
---|
| 1244 | S /= h[k]**(7.0/3) |
---|
| 1245 | |
---|
| 1246 | #Update momentum |
---|
| 1247 | xmom_update[k] += S*uh[k] |
---|
| 1248 | ymom_update[k] += S*vh[k] |
---|
| 1249 | |
---|
| 1250 | |
---|
| 1251 | def manning_friction_c(domain): |
---|
| 1252 | """Wrapper for c version |
---|
| 1253 | """ |
---|
| 1254 | |
---|
| 1255 | |
---|
| 1256 | xmom = domain.quantities['xmomentum'] |
---|
| 1257 | ymom = domain.quantities['ymomentum'] |
---|
| 1258 | |
---|
| 1259 | w = domain.quantities['stage'].centroid_values |
---|
| 1260 | z = domain.quantities['elevation'].centroid_values |
---|
| 1261 | |
---|
| 1262 | uh = xmom.centroid_values |
---|
| 1263 | vh = ymom.centroid_values |
---|
| 1264 | eta = domain.quantities['friction'].centroid_values |
---|
| 1265 | |
---|
| 1266 | xmom_update = xmom.semi_implicit_update |
---|
| 1267 | ymom_update = ymom.semi_implicit_update |
---|
| 1268 | |
---|
| 1269 | N = domain.number_of_elements |
---|
| 1270 | eps = domain.minimum_allowed_height |
---|
| 1271 | g = domain.g |
---|
| 1272 | |
---|
| 1273 | from shallow_water_ext import manning_friction |
---|
| 1274 | manning_friction(g, eps, w, z, uh, vh, eta, xmom_update, ymom_update) |
---|
| 1275 | |
---|
| 1276 | |
---|
| 1277 | def linear_friction(domain): |
---|
| 1278 | """Apply linear friction to water momentum |
---|
| 1279 | |
---|
| 1280 | Assumes quantity: 'linear_friction' to be present |
---|
| 1281 | """ |
---|
| 1282 | |
---|
| 1283 | from math import sqrt |
---|
| 1284 | |
---|
| 1285 | w = domain.quantities['stage'].centroid_values |
---|
| 1286 | z = domain.quantities['elevation'].centroid_values |
---|
| 1287 | h = w-z |
---|
| 1288 | |
---|
| 1289 | uh = domain.quantities['xmomentum'].centroid_values |
---|
| 1290 | vh = domain.quantities['ymomentum'].centroid_values |
---|
| 1291 | tau = domain.quantities['linear_friction'].centroid_values |
---|
| 1292 | |
---|
| 1293 | xmom_update = domain.quantities['xmomentum'].semi_implicit_update |
---|
| 1294 | ymom_update = domain.quantities['ymomentum'].semi_implicit_update |
---|
| 1295 | |
---|
| 1296 | N = domain.number_of_elements |
---|
| 1297 | eps = domain.minimum_allowed_height |
---|
| 1298 | g = domain.g #Not necessary? Why was this added? |
---|
| 1299 | |
---|
| 1300 | for k in range(N): |
---|
| 1301 | if tau[k] >= eps: |
---|
| 1302 | if h[k] >= eps: |
---|
| 1303 | S = -tau[k]/h[k] |
---|
| 1304 | |
---|
| 1305 | #Update momentum |
---|
| 1306 | xmom_update[k] += S*uh[k] |
---|
| 1307 | ymom_update[k] += S*vh[k] |
---|
| 1308 | |
---|
| 1309 | |
---|
| 1310 | |
---|
| 1311 | def check_forcefield(f): |
---|
| 1312 | """Check that f is either |
---|
| 1313 | 1: a callable object f(t,x,y), where x and y are vectors |
---|
| 1314 | and that it returns an array or a list of same length |
---|
| 1315 | as x and y |
---|
| 1316 | 2: a scalar |
---|
| 1317 | """ |
---|
| 1318 | |
---|
| 1319 | from Numeric import ones, Float, array |
---|
| 1320 | |
---|
| 1321 | |
---|
| 1322 | if callable(f): |
---|
| 1323 | N = 3 |
---|
| 1324 | x = ones(3, Float) |
---|
| 1325 | y = ones(3, Float) |
---|
| 1326 | try: |
---|
| 1327 | q = f(1.0, x=x, y=y) |
---|
| 1328 | except Exception, e: |
---|
| 1329 | msg = 'Function %s could not be executed:\n%s' %(f, e) |
---|
| 1330 | #FIXME: Reconsider this semantics |
---|
| 1331 | raise msg |
---|
| 1332 | |
---|
| 1333 | try: |
---|
| 1334 | q = array(q).astype(Float) |
---|
| 1335 | except: |
---|
| 1336 | msg = 'Return value from vector function %s could ' %f |
---|
| 1337 | msg += 'not be converted into a Numeric array of floats.\n' |
---|
| 1338 | msg += 'Specified function should return either list or array.' |
---|
| 1339 | raise msg |
---|
| 1340 | |
---|
| 1341 | #Is this really what we want? |
---|
| 1342 | msg = 'Return vector from function %s ' %f |
---|
| 1343 | msg += 'must have same lenght as input vectors' |
---|
| 1344 | assert len(q) == N, msg |
---|
| 1345 | |
---|
| 1346 | else: |
---|
| 1347 | try: |
---|
| 1348 | f = float(f) |
---|
| 1349 | except: |
---|
| 1350 | msg = 'Force field %s must be either a scalar' %f |
---|
| 1351 | msg += ' or a vector function' |
---|
| 1352 | raise msg |
---|
| 1353 | return f |
---|
| 1354 | |
---|
| 1355 | |
---|
| 1356 | class Wind_stress: |
---|
| 1357 | """Apply wind stress to water momentum in terms of |
---|
| 1358 | wind speed [m/s] and wind direction [degrees] |
---|
| 1359 | """ |
---|
| 1360 | |
---|
| 1361 | def __init__(self, *args, **kwargs): |
---|
| 1362 | """Initialise windfield from wind speed s [m/s] |
---|
| 1363 | and wind direction phi [degrees] |
---|
| 1364 | |
---|
| 1365 | Inputs v and phi can be either scalars or Python functions, e.g. |
---|
| 1366 | |
---|
| 1367 | W = Wind_stress(10, 178) |
---|
| 1368 | |
---|
| 1369 | #FIXME - 'normal' degrees are assumed for now, i.e. the |
---|
| 1370 | vector (1,0) has zero degrees. |
---|
| 1371 | We may need to convert from 'compass' degrees later on and also |
---|
| 1372 | map from True north to grid north. |
---|
| 1373 | |
---|
| 1374 | Arguments can also be Python functions of t,x,y as in |
---|
| 1375 | |
---|
| 1376 | def speed(t,x,y): |
---|
| 1377 | ... |
---|
| 1378 | return s |
---|
| 1379 | |
---|
| 1380 | def angle(t,x,y): |
---|
| 1381 | ... |
---|
| 1382 | return phi |
---|
| 1383 | |
---|
| 1384 | where x and y are vectors. |
---|
| 1385 | |
---|
| 1386 | and then pass the functions in |
---|
| 1387 | |
---|
| 1388 | W = Wind_stress(speed, angle) |
---|
| 1389 | |
---|
| 1390 | The instantiated object W can be appended to the list of |
---|
| 1391 | forcing_terms as in |
---|
| 1392 | |
---|
| 1393 | Alternatively, one vector valued function for (speed, angle) |
---|
| 1394 | can be applied, providing both quantities simultaneously. |
---|
| 1395 | As in |
---|
| 1396 | W = Wind_stress(F), where returns (speed, angle) for each t. |
---|
| 1397 | |
---|
| 1398 | domain.forcing_terms.append(W) |
---|
| 1399 | """ |
---|
| 1400 | |
---|
| 1401 | from config import rho_a, rho_w, eta_w |
---|
| 1402 | from Numeric import array, Float |
---|
| 1403 | |
---|
| 1404 | if len(args) == 2: |
---|
| 1405 | s = args[0] |
---|
| 1406 | phi = args[1] |
---|
| 1407 | elif len(args) == 1: |
---|
| 1408 | #Assume vector function returning (s, phi)(t,x,y) |
---|
| 1409 | vector_function = args[0] |
---|
| 1410 | s = lambda t,x,y: vector_function(t,x=x,y=y)[0] |
---|
| 1411 | phi = lambda t,x,y: vector_function(t,x=x,y=y)[1] |
---|
| 1412 | else: |
---|
| 1413 | #Assume info is in 2 keyword arguments |
---|
| 1414 | |
---|
| 1415 | if len(kwargs) == 2: |
---|
| 1416 | s = kwargs['s'] |
---|
| 1417 | phi = kwargs['phi'] |
---|
| 1418 | else: |
---|
| 1419 | raise 'Assumes two keyword arguments: s=..., phi=....' |
---|
| 1420 | |
---|
| 1421 | self.speed = check_forcefield(s) |
---|
| 1422 | self.phi = check_forcefield(phi) |
---|
| 1423 | |
---|
| 1424 | self.const = eta_w*rho_a/rho_w |
---|
| 1425 | |
---|
| 1426 | |
---|
| 1427 | def __call__(self, domain): |
---|
| 1428 | """Evaluate windfield based on values found in domain |
---|
| 1429 | """ |
---|
| 1430 | |
---|
| 1431 | from math import pi, cos, sin, sqrt |
---|
| 1432 | from Numeric import Float, ones, ArrayType |
---|
| 1433 | |
---|
| 1434 | xmom_update = domain.quantities['xmomentum'].explicit_update |
---|
| 1435 | ymom_update = domain.quantities['ymomentum'].explicit_update |
---|
| 1436 | |
---|
| 1437 | N = domain.number_of_elements |
---|
| 1438 | t = domain.time |
---|
| 1439 | |
---|
| 1440 | if callable(self.speed): |
---|
| 1441 | xc = domain.get_centroid_coordinates() |
---|
| 1442 | s_vec = self.speed(t, xc[:,0], xc[:,1]) |
---|
| 1443 | else: |
---|
| 1444 | #Assume s is a scalar |
---|
| 1445 | |
---|
| 1446 | try: |
---|
| 1447 | s_vec = self.speed * ones(N, Float) |
---|
| 1448 | except: |
---|
| 1449 | msg = 'Speed must be either callable or a scalar: %s' %self.s |
---|
| 1450 | raise msg |
---|
| 1451 | |
---|
| 1452 | |
---|
| 1453 | if callable(self.phi): |
---|
| 1454 | xc = domain.get_centroid_coordinates() |
---|
| 1455 | phi_vec = self.phi(t, xc[:,0], xc[:,1]) |
---|
| 1456 | else: |
---|
| 1457 | #Assume phi is a scalar |
---|
| 1458 | |
---|
| 1459 | try: |
---|
| 1460 | phi_vec = self.phi * ones(N, Float) |
---|
| 1461 | except: |
---|
| 1462 | msg = 'Angle must be either callable or a scalar: %s' %self.phi |
---|
| 1463 | raise msg |
---|
| 1464 | |
---|
| 1465 | assign_windfield_values(xmom_update, ymom_update, |
---|
| 1466 | s_vec, phi_vec, self.const) |
---|
| 1467 | |
---|
| 1468 | |
---|
| 1469 | def assign_windfield_values(xmom_update, ymom_update, |
---|
| 1470 | s_vec, phi_vec, const): |
---|
| 1471 | """Python version of assigning wind field to update vectors. |
---|
| 1472 | A c version also exists (for speed) |
---|
| 1473 | """ |
---|
| 1474 | from math import pi, cos, sin, sqrt |
---|
| 1475 | |
---|
| 1476 | N = len(s_vec) |
---|
| 1477 | for k in range(N): |
---|
| 1478 | s = s_vec[k] |
---|
| 1479 | phi = phi_vec[k] |
---|
| 1480 | |
---|
| 1481 | #Convert to radians |
---|
| 1482 | phi = phi*pi/180 |
---|
| 1483 | |
---|
| 1484 | #Compute velocity vector (u, v) |
---|
| 1485 | u = s*cos(phi) |
---|
| 1486 | v = s*sin(phi) |
---|
| 1487 | |
---|
| 1488 | #Compute wind stress |
---|
| 1489 | S = const * sqrt(u**2 + v**2) |
---|
| 1490 | xmom_update[k] += S*u |
---|
| 1491 | ymom_update[k] += S*v |
---|
| 1492 | |
---|
| 1493 | |
---|
| 1494 | |
---|
| 1495 | ############################## |
---|
| 1496 | #OBSOLETE STUFF |
---|
| 1497 | |
---|
| 1498 | def balance_deep_and_shallow_old(domain): |
---|
| 1499 | """Compute linear combination between stage as computed by |
---|
| 1500 | gradient-limiters and stage computed as constant height above bed. |
---|
| 1501 | The former takes precedence when heights are large compared to the |
---|
| 1502 | bed slope while the latter takes precedence when heights are |
---|
| 1503 | relatively small. Anything in between is computed as a balanced |
---|
| 1504 | linear combination in order to avoid numerical disturbances which |
---|
| 1505 | would otherwise appear as a result of hard switching between |
---|
| 1506 | modes. |
---|
| 1507 | """ |
---|
| 1508 | |
---|
| 1509 | #OBSOLETE |
---|
| 1510 | |
---|
| 1511 | #Shortcuts |
---|
| 1512 | wc = domain.quantities['stage'].centroid_values |
---|
| 1513 | zc = domain.quantities['elevation'].centroid_values |
---|
| 1514 | hc = wc - zc |
---|
| 1515 | |
---|
| 1516 | wv = domain.quantities['stage'].vertex_values |
---|
| 1517 | zv = domain.quantities['elevation'].vertex_values |
---|
| 1518 | hv = wv-zv |
---|
| 1519 | |
---|
| 1520 | |
---|
| 1521 | #Computed linear combination between constant stages and and |
---|
| 1522 | #stages parallel to the bed elevation. |
---|
| 1523 | for k in range(domain.number_of_elements): |
---|
| 1524 | #Compute maximal variation in bed elevation |
---|
| 1525 | # This quantitiy is |
---|
| 1526 | # dz = max_i abs(z_i - z_c) |
---|
| 1527 | # and it is independent of dimension |
---|
| 1528 | # In the 1d case zc = (z0+z1)/2 |
---|
| 1529 | # In the 2d case zc = (z0+z1+z2)/3 |
---|
| 1530 | |
---|
| 1531 | dz = max(abs(zv[k,0]-zc[k]), |
---|
| 1532 | abs(zv[k,1]-zc[k]), |
---|
| 1533 | abs(zv[k,2]-zc[k])) |
---|
| 1534 | |
---|
| 1535 | |
---|
| 1536 | hmin = min( hv[k,:] ) |
---|
| 1537 | |
---|
| 1538 | #Create alpha in [0,1], where alpha==0 means using shallow |
---|
| 1539 | #first order scheme and alpha==1 means using the stage w as |
---|
| 1540 | #computed by the gradient limiter (1st or 2nd order) |
---|
| 1541 | # |
---|
| 1542 | #If hmin > dz/2 then alpha = 1 and the bed will have no effect |
---|
| 1543 | #If hmin < 0 then alpha = 0 reverting to constant height above bed. |
---|
| 1544 | |
---|
| 1545 | if dz > 0.0: |
---|
| 1546 | alpha = max( min( 2*hmin/dz, 1.0), 0.0 ) |
---|
| 1547 | else: |
---|
| 1548 | #Flat bed |
---|
| 1549 | alpha = 1.0 |
---|
| 1550 | |
---|
| 1551 | #Weighted balance between stage parallel to bed elevation |
---|
| 1552 | #(wvi = zvi + hc) and stage as computed by 1st or 2nd |
---|
| 1553 | #order gradient limiter |
---|
| 1554 | #(wvi = zvi + hvi) where i=0,1,2 denotes the vertex ids |
---|
| 1555 | # |
---|
| 1556 | #It follows that the updated wvi is |
---|
| 1557 | # wvi := (1-alpha)*(zvi+hc) + alpha*(zvi+hvi) = |
---|
| 1558 | # zvi + hc + alpha*(hvi - hc) |
---|
| 1559 | # |
---|
| 1560 | #Note that hvi = zc+hc-zvi in the first order case (constant). |
---|
| 1561 | |
---|
| 1562 | if alpha < 1: |
---|
| 1563 | for i in range(3): |
---|
| 1564 | wv[k,i] = zv[k,i] + hc[k] + alpha*(hv[k,i]-hc[k]) |
---|
| 1565 | |
---|
| 1566 | |
---|
| 1567 | #Momentums at centroids |
---|
| 1568 | xmomc = domain.quantities['xmomentum'].centroid_values |
---|
| 1569 | ymomc = domain.quantities['ymomentum'].centroid_values |
---|
| 1570 | |
---|
| 1571 | #Momentums at vertices |
---|
| 1572 | xmomv = domain.quantities['xmomentum'].vertex_values |
---|
| 1573 | ymomv = domain.quantities['ymomentum'].vertex_values |
---|
| 1574 | |
---|
| 1575 | # Update momentum as a linear combination of |
---|
| 1576 | # xmomc and ymomc (shallow) and momentum |
---|
| 1577 | # from extrapolator xmomv and ymomv (deep). |
---|
| 1578 | xmomv[k,:] = (1-alpha)*xmomc[k] + alpha*xmomv[k,:] |
---|
| 1579 | ymomv[k,:] = (1-alpha)*ymomc[k] + alpha*ymomv[k,:] |
---|
| 1580 | |
---|
| 1581 | |
---|
| 1582 | |
---|
| 1583 | |
---|
| 1584 | |
---|
| 1585 | ########################### |
---|
| 1586 | ########################### |
---|
| 1587 | #Geometries |
---|
| 1588 | |
---|
| 1589 | |
---|
| 1590 | #FIXME: Rethink this way of creating values. |
---|
| 1591 | |
---|
| 1592 | |
---|
| 1593 | class Weir: |
---|
| 1594 | """Set a bathymetry for weir with a hole and a downstream gutter |
---|
| 1595 | x,y are assumed to be in the unit square |
---|
| 1596 | """ |
---|
| 1597 | |
---|
| 1598 | def __init__(self, stage): |
---|
| 1599 | self.inflow_stage = stage |
---|
| 1600 | |
---|
| 1601 | def __call__(self, x, y): |
---|
| 1602 | from Numeric import zeros, Float |
---|
| 1603 | from math import sqrt |
---|
| 1604 | |
---|
| 1605 | N = len(x) |
---|
| 1606 | assert N == len(y) |
---|
| 1607 | |
---|
| 1608 | z = zeros(N, Float) |
---|
| 1609 | for i in range(N): |
---|
| 1610 | z[i] = -x[i]/2 #General slope |
---|
| 1611 | |
---|
| 1612 | #Flattish bit to the left |
---|
| 1613 | if x[i] < 0.3: |
---|
| 1614 | z[i] = -x[i]/10 |
---|
| 1615 | |
---|
| 1616 | #Weir |
---|
| 1617 | if x[i] >= 0.3 and x[i] < 0.4: |
---|
| 1618 | z[i] = -x[i]+0.9 |
---|
| 1619 | |
---|
| 1620 | #Dip |
---|
| 1621 | x0 = 0.6 |
---|
| 1622 | #depth = -1.3 |
---|
| 1623 | depth = -1.0 |
---|
| 1624 | #plateaux = -0.9 |
---|
| 1625 | plateaux = -0.6 |
---|
| 1626 | if y[i] < 0.7: |
---|
| 1627 | if x[i] > x0 and x[i] < 0.9: |
---|
| 1628 | z[i] = depth |
---|
| 1629 | |
---|
| 1630 | #RHS plateaux |
---|
| 1631 | if x[i] >= 0.9: |
---|
| 1632 | z[i] = plateaux |
---|
| 1633 | |
---|
| 1634 | |
---|
| 1635 | elif y[i] >= 0.7 and y[i] < 1.5: |
---|
| 1636 | #Restrict and deepen |
---|
| 1637 | if x[i] >= x0 and x[i] < 0.8: |
---|
| 1638 | z[i] = depth-(y[i]/3-0.3) |
---|
| 1639 | #z[i] = depth-y[i]/5 |
---|
| 1640 | #z[i] = depth |
---|
| 1641 | elif x[i] >= 0.8: |
---|
| 1642 | #RHS plateaux |
---|
| 1643 | z[i] = plateaux |
---|
| 1644 | |
---|
| 1645 | elif y[i] >= 1.5: |
---|
| 1646 | if x[i] >= x0 and x[i] < 0.8 + (y[i]-1.5)/1.2: |
---|
| 1647 | #Widen up and stay at constant depth |
---|
| 1648 | z[i] = depth-1.5/5 |
---|
| 1649 | elif x[i] >= 0.8 + (y[i]-1.5)/1.2: |
---|
| 1650 | #RHS plateaux |
---|
| 1651 | z[i] = plateaux |
---|
| 1652 | |
---|
| 1653 | |
---|
| 1654 | #Hole in weir (slightly higher than inflow condition) |
---|
| 1655 | if x[i] >= 0.3 and x[i] < 0.4 and y[i] > 0.2 and y[i] < 0.4: |
---|
| 1656 | z[i] = -x[i]+self.inflow_stage + 0.02 |
---|
| 1657 | |
---|
| 1658 | #Channel behind weir |
---|
| 1659 | x0 = 0.5 |
---|
| 1660 | if x[i] >= 0.4 and x[i] < x0 and y[i] > 0.2 and y[i] < 0.4: |
---|
| 1661 | z[i] = -x[i]+self.inflow_stage + 0.02 |
---|
| 1662 | |
---|
| 1663 | if x[i] >= x0 and x[i] < 0.6 and y[i] > 0.2 and y[i] < 0.4: |
---|
| 1664 | #Flatten it out towards the end |
---|
| 1665 | z[i] = -x0+self.inflow_stage + 0.02 + (x0-x[i])/5 |
---|
| 1666 | |
---|
| 1667 | #Hole to the east |
---|
| 1668 | x0 = 1.1; y0 = 0.35 |
---|
| 1669 | #if x[i] < -0.2 and y < 0.5: |
---|
| 1670 | if sqrt((2*(x[i]-x0))**2 + (2*(y[i]-y0))**2) < 0.2: |
---|
| 1671 | z[i] = sqrt(((x[i]-x0))**2 + ((y[i]-y0))**2)-1.0 |
---|
| 1672 | |
---|
| 1673 | #Tiny channel draining hole |
---|
| 1674 | if x[i] >= 1.14 and x[i] < 1.2 and y[i] >= 0.4 and y[i] < 0.6: |
---|
| 1675 | z[i] = -0.9 #North south |
---|
| 1676 | |
---|
| 1677 | if x[i] >= 0.9 and x[i] < 1.18 and y[i] >= 0.58 and y[i] < 0.65: |
---|
| 1678 | z[i] = -1.0 + (x[i]-0.9)/3 #East west |
---|
| 1679 | |
---|
| 1680 | |
---|
| 1681 | |
---|
| 1682 | #Stuff not in use |
---|
| 1683 | |
---|
| 1684 | #Upward slope at inlet to the north west |
---|
| 1685 | #if x[i] < 0.0: # and y[i] > 0.5: |
---|
| 1686 | # #z[i] = -y[i]+0.5 #-x[i]/2 |
---|
| 1687 | # z[i] = x[i]/4 - y[i]**2 + 0.5 |
---|
| 1688 | |
---|
| 1689 | #Hole to the west |
---|
| 1690 | #x0 = -0.4; y0 = 0.35 # center |
---|
| 1691 | #if sqrt((2*(x[i]-x0))**2 + (2*(y[i]-y0))**2) < 0.2: |
---|
| 1692 | # z[i] = sqrt(((x[i]-x0))**2 + ((y[i]-y0))**2)-0.2 |
---|
| 1693 | |
---|
| 1694 | |
---|
| 1695 | |
---|
| 1696 | |
---|
| 1697 | |
---|
| 1698 | return z/2 |
---|
| 1699 | |
---|
| 1700 | class Weir_simple: |
---|
| 1701 | """Set a bathymetry for weir with a hole and a downstream gutter |
---|
| 1702 | x,y are assumed to be in the unit square |
---|
| 1703 | """ |
---|
| 1704 | |
---|
| 1705 | def __init__(self, stage): |
---|
| 1706 | self.inflow_stage = stage |
---|
| 1707 | |
---|
| 1708 | def __call__(self, x, y): |
---|
| 1709 | from Numeric import zeros, Float |
---|
| 1710 | |
---|
| 1711 | N = len(x) |
---|
| 1712 | assert N == len(y) |
---|
| 1713 | |
---|
| 1714 | z = zeros(N, Float) |
---|
| 1715 | for i in range(N): |
---|
| 1716 | z[i] = -x[i] #General slope |
---|
| 1717 | |
---|
| 1718 | #Flat bit to the left |
---|
| 1719 | if x[i] < 0.3: |
---|
| 1720 | z[i] = -x[i]/10 #General slope |
---|
| 1721 | |
---|
| 1722 | #Weir |
---|
| 1723 | if x[i] > 0.3 and x[i] < 0.4: |
---|
| 1724 | z[i] = -x[i]+0.9 |
---|
| 1725 | |
---|
| 1726 | #Dip |
---|
| 1727 | if x[i] > 0.6 and x[i] < 0.9: |
---|
| 1728 | z[i] = -x[i]-0.5 #-y[i]/5 |
---|
| 1729 | |
---|
| 1730 | #Hole in weir (slightly higher than inflow condition) |
---|
| 1731 | if x[i] > 0.3 and x[i] < 0.4 and y[i] > 0.2 and y[i] < 0.4: |
---|
| 1732 | z[i] = -x[i]+self.inflow_stage + 0.05 |
---|
| 1733 | |
---|
| 1734 | |
---|
| 1735 | return z/2 |
---|
| 1736 | |
---|
| 1737 | |
---|
| 1738 | |
---|
| 1739 | class Constant_stage: |
---|
| 1740 | """Set an initial condition with constant stage |
---|
| 1741 | """ |
---|
| 1742 | def __init__(self, s): |
---|
| 1743 | self.s = s |
---|
| 1744 | |
---|
| 1745 | def __call__(self, x, y): |
---|
| 1746 | return self.s |
---|
| 1747 | |
---|
| 1748 | class Constant_height: |
---|
| 1749 | """Set an initial condition with constant water height, e.g |
---|
| 1750 | stage s = z+h |
---|
| 1751 | """ |
---|
| 1752 | |
---|
| 1753 | def __init__(self, W, h): |
---|
| 1754 | self.W = W |
---|
| 1755 | self.h = h |
---|
| 1756 | |
---|
| 1757 | def __call__(self, x, y): |
---|
| 1758 | if self.W is None: |
---|
| 1759 | from Numeric import ones, Float |
---|
| 1760 | return self.h*ones(len(x), Float) |
---|
| 1761 | else: |
---|
| 1762 | return self.W(x,y) + self.h |
---|
| 1763 | |
---|
| 1764 | |
---|
| 1765 | |
---|
| 1766 | |
---|
| 1767 | |
---|
| 1768 | |
---|
| 1769 | |
---|
| 1770 | ############################################## |
---|
| 1771 | #Initialise module |
---|
| 1772 | |
---|
| 1773 | |
---|
| 1774 | from utilities import compile |
---|
| 1775 | if compile.can_use_C_extension('shallow_water_kinetic_ext.c'): |
---|
| 1776 | #Replace python version with c implementations |
---|
| 1777 | |
---|
| 1778 | from shallow_water_kinetic_ext import rotate, assign_windfield_values |
---|
| 1779 | compute_fluxes = compute_fluxes_c |
---|
| 1780 | extrapolate_second_order_sw=extrapolate_second_order_sw_c |
---|
| 1781 | gravity = gravity_c |
---|
| 1782 | manning_friction = manning_friction_c |
---|
| 1783 | h_limiter = h_limiter_c |
---|
| 1784 | balance_deep_and_shallow = balance_deep_and_shallow_c |
---|
| 1785 | protect_against_infinitesimal_and_negative_heights = protect_against_infinitesimal_and_negative_heights_c |
---|
| 1786 | |
---|
| 1787 | |
---|
| 1788 | #distribute_to_vertices_and_edges = distribute_to_vertices_and_edges_c #(like MH's) |
---|
| 1789 | |
---|
| 1790 | |
---|
| 1791 | |
---|
| 1792 | #Optimisation with psyco |
---|
| 1793 | from config import use_psyco |
---|
| 1794 | if use_psyco: |
---|
| 1795 | try: |
---|
| 1796 | import psyco |
---|
| 1797 | except: |
---|
| 1798 | import os |
---|
| 1799 | if os.name == 'posix' and os.uname()[4] == 'x86_64': |
---|
| 1800 | pass |
---|
| 1801 | #Psyco isn't supported on 64 bit systems, but it doesn't matter |
---|
| 1802 | else: |
---|
| 1803 | msg = 'WARNING: psyco (speedup) could not import'+\ |
---|
| 1804 | ', you may want to consider installing it' |
---|
| 1805 | print msg |
---|
| 1806 | else: |
---|
| 1807 | psyco.bind(Domain.distribute_to_vertices_and_edges) |
---|
| 1808 | psyco.bind(Domain.compute_fluxes) |
---|
| 1809 | |
---|
| 1810 | if __name__ == "__main__": |
---|
| 1811 | pass |
---|
| 1812 | |
---|
| 1813 | # Profiling stuff |
---|
| 1814 | import profile |
---|
| 1815 | profiler = profile.Profile() |
---|