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Secondary circulation

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involves an in-up-out secondary circulation flow that is also important to its clouds and rain. On a planetary scale, Earth's winds are mostly east–west or
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that contains most of the kinetic energy and momentum of a flow. For example, a
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is a weak circulation that plays a key maintenance role in sustaining a stronger
235: 24: 227: 208: 145: 284: 188: 18: 357: 300: 243: 46: 140:, but that flow is maintained against friction by the 130:tropical cyclone's primary winds are tangential 377: 320: 263: 8: 51:introducing citations to additional sources 384: 370: 327: 313: 270: 256: 134:evolution and maintenance against friction 41:Relevant discussion may be found on the 16:Circulation induced in a rotating system 179: 190:An introduction to dynamic meteorology 7: 338: 336: 281: 279: 224: 222: 356:. You can help Knowledge (XXG) by 299:. You can help Knowledge (XXG) by 242:. You can help Knowledge (XXG) by 14: 144:acting on a small north–south or 132:(horizontally swirling), but its 340: 283: 226: 34:relies largely or entirely on a 23: 1: 449: 335: 278: 221: 187:Holton, James R. (2019). 148:secondary circulation. 62:"Secondary circulation" 352:–related article is a 238:–related article is a 408:Physical oceanography 116:secondary circulation 114:In fluid dynamics, a 433:Fluid dynamics stubs 413:Atmospheric dynamics 193:. Elsevier Science. 47:improve this article 163:Primitive equations 126:primary circulation 428:Oceanography stubs 423:Meteorology stubs 365: 364: 308: 307: 251: 250: 112: 111: 97: 440: 386: 379: 372: 344: 337: 329: 322: 315: 287: 280: 272: 265: 258: 230: 223: 213: 212: 184: 107: 104: 98: 96: 55: 27: 19: 448: 447: 443: 442: 441: 439: 438: 437: 418:Fluid mechanics 393: 392: 391: 390: 334: 333: 277: 276: 219: 217: 216: 201: 186: 185: 181: 176: 154: 108: 102: 99: 56: 54: 40: 28: 17: 12: 11: 5: 446: 444: 436: 435: 430: 425: 420: 415: 410: 405: 395: 394: 389: 388: 381: 374: 366: 363: 362: 350:fluid dynamics 345: 332: 331: 324: 317: 309: 306: 305: 288: 275: 274: 267: 260: 252: 249: 248: 231: 215: 214: 199: 178: 177: 175: 172: 171: 170: 168:Secondary flow 165: 160: 158:Hough function 153: 150: 142:Coriolis force 121:secondary flow 110: 109: 45:. Please help 31: 29: 22: 15: 13: 10: 9: 6: 4: 3: 2: 445: 434: 431: 429: 426: 424: 421: 419: 416: 414: 411: 409: 406: 404: 401: 400: 398: 387: 382: 380: 375: 373: 368: 367: 361: 359: 355: 351: 346: 343: 339: 330: 325: 323: 318: 316: 311: 310: 304: 302: 298: 295:article is a 294: 289: 286: 282: 273: 268: 266: 261: 259: 254: 253: 247: 245: 241: 237: 232: 229: 225: 220: 210: 206: 202: 200:9780128093290 196: 192: 191: 183: 180: 173: 169: 166: 164: 161: 159: 156: 155: 151: 149: 147: 143: 139: 135: 131: 127: 123: 122: 117: 106: 103:December 2019 95: 92: 88: 85: 81: 78: 74: 71: 67: 64: â€“  63: 59: 58:Find sources: 52: 48: 44: 38: 37: 36:single source 32:This article 30: 26: 21: 20: 358:expanding it 347: 301:expanding it 293:oceanography 290: 244:expanding it 233: 218: 189: 182: 125: 119: 115: 113: 100: 90: 83: 76: 69: 57: 33: 236:meteorology 403:Geophysics 397:Categories 209:1124306270 174:References 146:meridional 73:newspapers 43:talk page 152:See also 87:scholar 207:  197:  89:  82:  75:  68:  60:  348:This 291:This 234:This 138:zonal 94:JSTOR 80:books 354:stub 297:stub 240:stub 205:OCLC 195:ISBN 66:news 118:or 49:by 399:: 203:. 385:e 378:t 371:v 360:. 328:e 321:t 314:v 303:. 271:e 264:t 257:v 246:. 211:. 105:) 101:( 91:· 84:· 77:· 70:· 53:. 39:.

Index


single source
talk page
improve this article
introducing citations to additional sources
"Secondary circulation"
news
newspapers
books
scholar
JSTOR
secondary flow
tropical cyclone's primary winds are tangential
evolution and maintenance against friction
zonal
Coriolis force
meridional
Hough function
Primitive equations
Secondary flow
An introduction to dynamic meteorology
ISBN
9780128093290
OCLC
1124306270
Stub icon
meteorology
stub
expanding it
v

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