Knowledge (XXG)

June 4, 1993, derecho

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506: 483: 24: 333:(LI) of -6. The low level wind profile indicated little directional shear, but significant speed shear as present. The 1200 UTC PAH sounding indicated a mean wind of 250o at 25 kt. This is more than favorable for a squall line to produce significant damaging winds over a long period of time and a large area which is what a derecho is. 231:
In addition, widespread crop damage was reported in portions of Virginia and North Carolina due to very large hail and damaging winds. There were also several spin-up tornadoes confirmed in North Carolina. In Virginia, there were several reports of tornado sightings, but none were actually confirmed.
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Moderate to significant damage was observed along the path. The hardest hit area was in Lynchburg Virginia, where winds of 80 mph were recorded. Significant damages to homes were reported, with roofs being peeled and church steeples being toppled. In addition, numerous trees toppled caused 95%
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Portions of southern Virginia and northern North Carolina suffered the most severe known damage from this derecho. The strong winds blew across the Appalachian mountains, and into farmland. This caused significant crop damage in these farmland areas, as well as toppling numerous trees in forests.
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The derecho continued pushing eastward, and it eventually reached the Lynchburg, Virginia area, where the worst damage overall is reported. In Lynchburg, gusts of nearly 80 mph knocked over two church steeples, peeled back roofs and brick walls, damaged thousands of cars and toppled so many
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Gravity waves weaken considerably when capping is eliminated. Without trapping, the amplitudes of most gravity waves decrease rapidly. Accordingly, this derecho weakened considerably as it entered Ohio and West Virginia during the late afternoon after the capping had been eradicated by afternoon
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will cause the air to sink to its original position. Repetitive upward and downward motion beneath the inversion often induces gravity waves. Areas of high and low pressure, or components of a gravity wave (i.e., crests and troughs), often propagate with and maintain convection above the capped
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During the morning and early afternoon of 4 June 1993, a storm complex moved across southern Missouri, southern Illinois, western and central Kentucky, and northern middle Tennessee. An associated high precipitation (HP) supercell evolved into a derecho . The derecho moved slightly south of and
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at 1700 UTC and continued into eastern Kentucky, reaching Somerset at 1810 UTC. The derecho exited Kentucky by 2000 UTC and continued eastward through Ohio and West Virginia. By 0000 UTC, 5 June, the derecho had moved to northeast North Carolina, producing windespread wind damage.
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was on the south end of this system, and was moving to the south. By the 00z analysis, the squall line was in Virginia and North Carolina, with the outflow boundary extending from The North Carolina/Tennessee border to the islands of North Carolina and the far western
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Throughout the day, the main low pressure system continued moving slowly to the northeast. The stationary boundary which was due east at 12z became tilted a bit to the southeast while very slowly moving northward. The associated outflow boundary with the now mature
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damage. However, with widespread very large hail being present along the entire path of this derecho, there was significant hail damage being reported to vehicles, windows, and especially crops. The total damage cost exceeded 70 million dollars
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trees that power was cut to 95 percent of the city. At least 23 people were hurt by the falling trees, but no deaths were reported in the state. The damage in Lynchburg alone was estimated at $ 21 million at the time.
349:. Initial storm movement was from the west at 45 kt, although the bow echo complex quickly accelerated as it moved across southeast Missouri (50 kt) and western Kentucky, reaching PAH at 1525 UTC. The derecho reached 532: 116:
Significant damage to structures was reported, including peeled roofs and toppled church steeples. Numerous trees were damaged, causing widespread power outages. Crops were impacted by winds and hail.
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aloft. (The 1200 UTC PAH sounding indicated a strong inversion between the surface and 925 mb.) Gravity waves thrive near boundaries. Convergence near boundaries forces air to rise with
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at 1615 UTC, speed having increased to 70 kt. The derecho continued across central Kentucky and northern middle Tennessee, maintaining an average speed of 60 kt. The storm reached
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parallel to a surface boundary along the Ohio River valley. This serial derecho produced widespread wind damage (and F0/F1 tornadoes) exceeding $ 70 million and injured 79.
623: 326: 216:. In addition, several severe wind reports were received scattered across this swath. In addition, there were a few weak 196:
swept across the Midwestern and Eastern United States. The most significant damage was reported in portions of southern
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along the cold front and southwest of the main low pressure. To the east of the low pressure, a
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The Governor of Virginia declared a state of emergency for this area due to the severe damage.
590: 386: 354: 277: 59: 533:"25 years ago: The windstorm that blasted Virginia when 'derecho' was still an obscure word" 350: 346: 281: 273: 249: 603: 406:
There was significant damage reported along the path. The primary damage type was mostly
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On the morning of June 4th, a storm complex was moving across the mid-west. At the 12z
213: 171: 373:, as suggested by the 60 kt movement of the derecho. The gravity wave developed in an 617: 161: 370: 358: 330: 293: 285: 253: 183: 92: 382: 322: 301: 220:
that were confirmed along the path. In addition, widespread large and damaging
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axis extended north to south across the southern plains states. The 1200 UTC
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The first report of wind damage was at 1345 UTC about 20 miles northwest of
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https://www.weather.gov/media/wrh/online_publications/talite/talite1406.pdf
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was analysed near the border of western Missouri and Arkansas. A large
551:"WPC North American surface analysis zoom, pan, animation and archives" 217: 193: 156: 204:. This derecho caused widespread wind damage reports in a swath from 261: 507:"SPC Historical Severe Weather Database Browser (SeverePlot 3.0)" 407: 221: 412: 276:
extended from this low and persisted due eastward across the
22: 526: 524: 522: 520: 531:Times-Dispatch, JOHN BOYER Richmond (4 June 2018). 120: 110: 99: 86: 78: 66: 51: 43: 35: 260:extended from the surface low southwestward into 58:100 mph (161 km/h; 44.7 m/s) ( 478: 476: 474: 268:. A cut-off low was also centered over Eastern 309:. The derecho was winding down by this point. 454: 452: 450: 448: 446: 444: 8: 16: 501: 499: 497: 15: 461:"An Analysis of Five Springtime Derechos" 440: 365:Although the derecho evolved from a HP 137: 599: 588: 484:"SeverePlot 3.0: Report data listing" 327:Convective Available Potential Energy 30:Wind and tornado reports for derecho. 7: 103: 14: 459:US Department of Commerce, NOAA. 228:of the city to be without power. 182:Most severe tornado damage; see 70:3.50 in (8.9 cm) ( 369:, it was likely sustained by a 292:that would be the foundational 1: 624:Derechos in the United States 329:(CAPE) of 1,838 J kg-1 and a 224:was observed along the path. 325:(KPAH) sounding indicated a 419:Virginia and North Carolina 317:At 1200 UTC, a weak 500 mb 288:was associated with the HP 640: 192:On June 4, 1993, a severe 72:Mocksville, North Carolina 415:) across the whole path. 247:Weather Prediction Center 180: 21: 125:Midwestern United States 537:Richmond Times-Dispatch 381:near the surface, with 236:Meteorological synopsis 88:Strongest tornado  296:for the main derecho. 208:eastward into much of 27: 313:Environmental factors 128:Eastern United States 112:Types of damage  26: 134:Provincial Breakdown 53:Peak wind gust  17:June 4, 1993 Derecho 565:"Derechos FAQ page" 18: 389:, and the lack of 212:into Virginia and 28: 598:Missing or empty 355:Bowling Green, KY 278:Ohio River Valley 190: 189: 186: 60:Elizabethtown, KY 631: 608: 607: 601: 596: 594: 586: 579: 573: 572: 569:www.spc.noaa.gov 561: 555: 554: 547: 541: 540: 528: 515: 514: 511:www.spc.noaa.gov 503: 492: 491: 488:www.spc.noaa.gov 480: 469: 468: 456: 351:Hopkinsville, KY 347:Poplar Bluff, MO 282:outflow boundary 274:stationary front 250:surface analysis 241:Surface features 181: 113: 105: 89: 62:, United States) 54: 19: 639: 638: 634: 633: 632: 630: 629: 628: 614: 613: 612: 611: 597: 587: 581: 580: 576: 563: 562: 558: 549: 548: 544: 530: 529: 518: 505: 504: 495: 482: 481: 472: 465:www.weather.gov 458: 457: 442: 437: 421: 404: 339: 315: 243: 238: 176: 136: 135: 130: 111: 87: 52: 31: 12: 11: 5: 637: 635: 627: 626: 616: 615: 610: 609: 574: 556: 542: 516: 493: 470: 439: 438: 436: 433: 420: 417: 403: 400: 338: 335: 314: 311: 307:Atlantic Ocean 242: 239: 237: 234: 214:North Carolina 188: 187: 178: 177: 175: 174: 172:North Carolina 169: 164: 159: 154: 149: 143: 133: 132: 131: 122: 121:Areas affected 118: 117: 114: 108: 107: 101: 97: 96: 90: 84: 83: 80: 76: 75: 68: 64: 63: 56: 49: 48: 45: 41: 40: 37: 33: 32: 29: 13: 10: 9: 6: 4: 3: 2: 636: 625: 622: 621: 619: 605: 592: 584: 578: 575: 570: 566: 560: 557: 552: 546: 543: 538: 534: 527: 525: 523: 521: 517: 512: 508: 502: 500: 498: 494: 489: 485: 479: 477: 475: 471: 466: 462: 455: 453: 451: 449: 447: 445: 441: 434: 432: 429: 425: 418: 416: 414: 409: 401: 399: 395: 392: 388: 384: 380: 376: 372: 368: 363: 360: 356: 352: 348: 343: 337:Derecho event 336: 334: 332: 328: 324: 320: 312: 310: 308: 303: 297: 295: 291: 287: 283: 279: 275: 271: 267: 263: 259: 255: 251: 248: 240: 235: 233: 229: 225: 223: 219: 215: 211: 207: 203: 200:, especially 199: 195: 185: 179: 173: 170: 168: 165: 163: 162:West Virginia 160: 158: 155: 153: 150: 147: 144: 141: 138: 129: 126: 123: 119: 115: 109: 102: 98: 94: 91: 85: 81: 79:Tornado count 77: 73: 69: 65: 61: 57: 50: 46: 42: 38: 34: 25: 20: 600:|title= 577: 568: 559: 545: 536: 510: 487: 464: 430: 426: 422: 405: 396: 371:gravity wave 364: 359:Gallatin, TN 344: 340: 331:lifted index 316: 298: 294:thunderstorm 286:triple point 254:low pressure 252:, a surface 244: 230: 226: 191: 184:Fujita scale 106:$ 70 million 100:Damage costs 67:Largest hail 39:June 4, 1993 383:instability 377:exhibiting 323:Paducah, KY 302:squall line 435:References 375:atmosphere 266:New Mexico 258:cold front 55:(measured) 398:heating. 379:stability 367:supercell 319:shortwave 290:supercell 284:near the 218:tornadoes 202:Lynchburg 618:Category 591:cite web 391:buoyancy 270:Oklahoma 210:Kentucky 206:Missouri 198:Virginia 167:Virginia 152:Kentucky 146:Illinois 140:Missouri 44:Duration 394:layer. 387:capping 194:derecho 157:Indiana 95:tornado 47:7 hours 36:Date(s) 402:Damage 280:. An 264:into 262:Texas 604:help 408:wind 222:hail 142:(SE) 104:est. 413:USD 148:(S) 620:: 595:: 593:}} 589:{{ 567:. 535:. 519:^ 509:. 496:^ 486:. 473:^ 463:. 443:^ 93:F1 82:12 606:) 602:( 585:. 571:. 553:. 539:. 513:. 490:. 467:. 411:( 357:/ 74:)

Index


Elizabethtown, KY
Mocksville, North Carolina
F1
Midwestern United States
Eastern United States
Missouri
Illinois
Kentucky
Indiana
West Virginia
Virginia
North Carolina
Fujita scale
derecho
Virginia
Lynchburg
Missouri
Kentucky
North Carolina
tornadoes
hail
Weather Prediction Center
surface analysis
low pressure
cold front
Texas
New Mexico
Oklahoma
stationary front

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