Online Book: "1001 Haby Hints for Meteorology and Weather Prediction" [--MAIN HOME--] [--HABY HINTS FACEBOOK PAGE--] SEARCH THIS SITE OR THE ENTIRE WEB WITH GOOGLE Enter your search terms Submit search form   Web www.theweatherprediction.com  Online Book: "1001 Haby Hints for Meteorology and Weather Prediction"  A link for each Weather Hint is below: 1. LOWER TROPOSPHERIC RELATIVE HUMIDITY 2. UPPER LEVEL LOWS 3. ADVECTION ASSOCIATED WITH MID-LATITUDE CYCLONES 4. THE FORECASTING OF DEW 5. THE FORECASTING OF FROST 6. OUTFLOW BOUNDARY CHARACTERISTICS 7. FORECASTING ICING ON ROADS 8. CHARACTERISTICS OF LOW-LYING FOG 9. DEW / FROST THICKNESS FUNCTIONS 10. THE IMPORTANCE OF FRICTION 11. THE SEA BREEZE 12. COLD FRONT MODIFICATION 13. MID-LATITUDE CYCLONE STRENGTHENING 14. PRESSURE TROUGHS AND SHORTWAVES 15. FORECASTING SYNOPTIC SCALE PRECIPITATION 16. DEWPOINT AS A FORECASTING TOOL 17. WIND AS A FORECASTING TOOL 18. CHANGES IN ATMOSPHERIC PRESSURE 19. UNDERSTANDING LATENT HEAT 20. IMPORTANT CLIMATOLOGICAL FACTORS 21. SOIL MOISTURE AND FORECASTING 22. RADIATION FOG INGREDIENTS 23. TORNADO SAFETY 24. LOWER TROPOSPHERIC ANALYSIS 25. FORECASTING USING THE 500 MILLIBAR CHART 26. JET STREAM ANALYSIS 27. CORIOLIS FORCE INTERPRETATION 28. CONTRIBUTING FACTORS TO INSTABILITY 29. BASIC EQUINOX DEFINITION 30. TEMPERATURE PROFILE OF THE TROPOSPHERE 31. SUPERADIABATIC LAPSE RATE 32. UPWIND AND DOWNWIND DEFINED 33. AN ADIABATIC VERSUS A DIABATIC PROCESS 34. ALBEDO AND THE ENERGY BUDGET 35. THE SOIL MOISTURE'S IMPACT ON WEATHER PREDICTION 36. THE 6 FACTORS THAT INFLUENCE HUMAN OUTSIDE COMFORT 37. METEOROLOGICAL SENSOR TYPES 38. ISOPLETHS DEFINED 39. THE DIFFERENCE BETWEEN TEMPERATURE AND HEAT 40. ATMOSPHERIC WATER VAPOR 41. WARMING AND COOLING OF THE EARTH'S SURFACE 42. SUPERCELL TYPES: LP, CLASSIC, HP 43. SEVERE WEATHER VERSUS FRONTAL TYPE 44. THE MOISTURE TONGUE DEFINED 45. (IN)STABILITY TYPES DEFINED 46. SEVERE WEATHER ENVIRONMENT 47. DOWNDRAFT TYPES: FORWARD FLANK AND REAR FLANK 48. VEERING AND BACKING WIND DEFINED 49. BAROTROPIC AND BAROCLINIC DEFINED 50. THE 3 MOTIONS WITHIN A TORNADO 51. VISIBILITY AND TORNADOES 52. RISING AIR PROCESSES AND PRODUCTS 53. THE HYDROLAPSE DEFINED 54. LIFTED INDEX INFORMATION 55. SEVERE WEATHER ENHANCERS 56. VORTICITY BASICS 57. FLASH FLOOD THREAT 58. TILTING OF TROUGHS ON A HORIZONTAL PLANE 59. DEWPOINT AND WETBULB DETAILS 60. FORECAST MODEL DATA INPUT 61. SMALL SCALE PRESSURE CHANGES 62. THE HYDROSTATIC EQUATION 63. SMALL SCALE WEATHER INFLUENCES 64. GRAVITY WAVE DEFINED 65. WHAT IS DPVA? 66. INCREASING FORECASTING KNOWLEDGE 67. ATTRIBUTES OF A BROADCAST METEOROLOGIST 68. THE PURPOSE OF A FORECAST 69. THE ART OF FORECASTING 70. FORECAST VERIFICATION 71. THE WINTER PRECIPITATION FORECAST 72. CATCHY PHRASES FOR BROADCAST METEOROLOGISTS 73. CONVERSIONS USING THE DOMINANT TEMPERATURE SCALES 74. KNOTS, PLUS OTHER WIND INFORMATION 75. THE FUNDAMENTALS OF Z TIME 76. THE DIFFERENCE BETWEEN ISOBARS AND ISOHYPSES 77. ASSESSING ATMOSPHERIC PRESSURES AND HEIGHTS 78. THE ISALLOBAR AND HEIGHT CHANGE CONTOURS 79. SURFACE VERSUS UPPER AIR STATION PLOTS 80. SNOW AND CLEAR SKIES 81. THE ART OF INTERPOLATION 82. LOCATING FRONTAL BOUNDARIES 83. USEFULNESS AND USELESSNESS OF RELATIVE HUMIDITY 84. THE IMPORTANCE OF EXPERIENCE AND BEING RESPECTED 85. WHAT CAUSES WIND? 86. MARITIME TROPICAL AIR MASS 87. MARITIME POLAR AIR MASS 88. DEDUCTIVE REASONING AND WEATHER FORECASTING 89. CONTINENTAL POLAR AIR MASS 90. CONTINENTAL TROPICAL AIR MASS 91. ARCTIC AIR MASS 92. HIGHLAND AIR MASS 93. TEACHING BASIC WEATHER 94. OCCLUDED FRONTS 95. USING MOS DATA 96. DYNAMIC SYNOPTIC SCALE RISING MOTION 97. THE 540 LINE AND PRECIPITATION TYPE 98. THE ZERO DEGREE ISOTHERM 99. THERMODYNAMIC INSTABILITY 100. RIDDING THE JET STREAM 101. VERTICAL VELOCITY ON THE 700 MB MODEL PROGS 102. THE 1000 MB FORECAST MODEL PROG 103. THE 850 MB MODEL PROG 104. THE 500 MB MODEL PROG 105. THE RELATIVE HUMIDITY PROG 106. THE LIFTED INDEX PROG 107. THE SURFACE PRESSURE/PRECIPITATION/THICKNESS PROG 108. THE 300 MILLIBAR PROG 109. USING MODEL PROGS FOR FORECASTING 110. THE GFS MODEL 111. DOWNSLOPING WIND 112. UPSLOPING WIND 113. EVALUATING TROPOSPHERIC MOISTURE 114. APPLYING TROPOSPHERIC MOISTURE TO FORECASTING 115. ANALYZING A STRONG LOW PRESSURE ON MODEL PROGS 116. ISENTROPIC LIFTING (UPGLIDE) 117. PET PEEVES AND BOTHERSOME METEOROLOGY 118. A LITTLE SUNSHINE MAKES A DIFFERENCE 119. CLOUDS ACT LIKE A BLANKET? 120. WHICH WAY IS UP? 121. WEATHER EXCITEMENT 122. THE DIFFERENT FORECAST MODELS 123. CHANGE IN PRESSURE, DENSITY AND TEMP. WITH HEIGHT 124. MELTING OF HAIL AS IT FALLS 125. WHAT IS A DIRTY HIGH PRESSURE? 126. WHAT IS AN INVERTED TROUGH? 127. WHAT IS A "NEGATIVELY TILTED TROUGH"? 128. WHAT IS MEANT BY A "VERTICALLY TILTED TROUGH"? 129. WHAT IS A LEE-SIDE TROUGH (LOW)? 130. WHAT IS A THERMAL TROUGH (RIDGE)? 131. WHAT IS A SHORTWAVE TROUGH? 132. WHAT DO THE TERMS DIGGING AND DEEPENING MEAN? 133. WHAT IS A SHEAR AXIS? 134. WHY DOES SURFACE CONV. OCCUR WITH LOW PRESSURE? 135. WHAT IS A CLASSIC EVENT? 136. WHAT IS A RETURN FLOW? 137. WHAT IS OMEGA FORCING? 138. DEFINING CHART, PANEL, PROG, ANALYSIS, IMAGE, MODEL, ect. 139. RED SKY IN MORNING, SAILORS WARNING 140. WEATHER AND MILITARY STRATEGY 141. INGREDIENTS FOR THUNDERSTORMS AND SEVERE STORMS 142. SOME PERSPECTIVE ON GRAVITY 143. DIFFERENT TERMS FOR A CHANGE IN TEMP. WITH HEIGHT 144. THE OMEGA BLOCK 145. NORTHERN HEMISPHERE MID-LATITUDE SEASONS 146. THUNDERSTORM OUTFLOW BOUNDARIES 147. CAPE AND LI USING GOES SOUNDER 148. READING THICKNESS LINES 149. HOW IS CONVERGENCE DISPLAYED ON THE GRAPHICAL MODELS? 150. WHAT IS A SQUALL LINE? 151. FORCE FIELDS AND DONUT HOLES 152. WAA VS. LOCAL HEATING ON THE 850 MB FORECAST MODELS 153. THE JET STREAM AND SUPERCELLS 154. A WEATHER FOLKLORE PHRASE INTERPRETED 155. CARBON DIOXIDE VS. WATER VAPOR AS GREENHOUSE GASES 156. WHY DOES THE PGF POINT FROM HIGH TO LOW PRESSURE? 157. WHAT IS A VARIABLE WIND? 158. THE INVERSION 159. ZONAL AND MERIDIONAL FLOW 160. THE DIFFERENCE BETWEEN THE LCL AND CCL 161. WHY THE MALR IS NOT A CONSTANT? 162. POTENTIAL TEMPERATURE AND THETA-E 163. NEGATIVE BOUYANCY AND THE CAP ON SKEW-T 164. ELEVATED CONVECTION 165. THE EL AND MPL 166. PREDICTING HAIL WITH THE SKEW-T 167. PREDICTING WINTER WEATHER WITH THE SKEW-T 168. THE HYDROLAPSE 169. OPERATIONAL USES OF THE LAYER SLICE METHOD 170. SHORTCUT TO CALCULATING WET-BULB 171. THE COL 172. FORECASTING SEVERE WEATHER USING SKEW-T 173. SATURATION VS. ACTUAL MIXING RATIO 174. HURRICANE INDUCED TORNADOES 175. WIND SHEAR AND SUPERCELLS 176. EXACT LOCATION OF THUNDERSTORM DEVELOPMENT 177. THE STORM PREDICTION CENTER'S CONVECTIVE OUTLOOKS 178. THE REX BLOCK 179. USING PERCENTAGES IN FORECASTS 180. LOCATING DOWNSLOPING AND UPSLOPE WIND on MODELS 181. READING FORECAST DISCUSSIONS 182. STAGES AND ATTAINMENT OF KNOWLEDGE 183. THE SOUND OF THUNDER 184. HOW DO CLOUDS DISSIPATE? 185. WHY DO MOST THUNDERSTORMS OCCUR IN LATE AFTERNOON? 186. CALCULATING RELATIVE HUMIDITY 187. WIDESPREAD VERSUS WIDELY SCATTERED 188. BOMBOGENESIS 189. CLOUD COVERAGE METHODS 190. EXPLAINING DEWPOINT AND HUMIDITY TO THE PUBLIC 191. THUNDERSTORM GLACIATION 192. WHY IS FOG MORE COMMON IN RURAL AREAS? 193. CALCULATING WINDSHEAR AND SHEAR VORTICITY 194. CALCULATION OF EARTH, SHEAR AND CURVATURE VORTICITY 195. INTERPRETATION OF UVV ON SYNOPTIC MODELS 196. EVAPORATIONAL COOLING 197. THE EFFECT OF VORTICITY ADVECTION ON HEIGHT CHANGE 198. THE VOLUME OF A RAINDROP 199. THE TEMPERATURE GRADIENT AND PRESSURE GRADIENT 200. THE CLOSED LOW 201. SNOW AND ICE ACCUMULATION (GRASS VERSUS CONCRETE) 202. SNOW AND ICE ACCUM. (INFLUENCE OF PREVIOUS WEATHER) 203. SNOW AND ICE ACCUMULATION (DAY VERSUS NIGHT) 204. SNOW ACCUM. (INFLUENCE FROM TEMPERATURE PROFILE) 205. SNOW AND ICE ACCUMULATION (INTENSITY AND DURATION) 206. THE SLEET STORM 207. THE COOLING EFFECTS OF SURFACE SNOW COVER 208. THE RATE OF A SNOWFLAKE MELTING AS IT FALLS 209. TYPES OF ICE TO SCRAPE OFF THE CAR 210. THE RATE AT WHICH RAIN FREEZES IN A FREEZING RAIN EVENT 211. MELTING RATE OF A SNOWFLAKE (ON WATER VS. LAND) 212. LEVEL IN THE TROPOSPHERE WITH GREATEST HEIGHT FALLS 213. LENGTH OF DAY AND NIGHT AT THE EQUINOXES 214. CONVECTIVE INSTABILITY DEFINITION AND EXAMPLE 215. WHY THE SUN AND MOON LOOK BIGGER NEAR THE HORIZON 216. COMPARING THE DENSITY OF AIR TO WATER 217. DEFINING A "VORT MAX" AND A "VORT LOBE" 218. HOW QUICKLY CAN PRECIPITATION SATURATE THE AIR? 219. SUNBURN / TANNING MYTHS EXPOSED 220. WHY IS THE TEMPERATURE AT 32 F DURING WET SNOW? 221. RAPID MORNING BAROTROPIC WARMING 222. CAN IT BE TOO COLD TO SNOW? 223. OPERATIONAL INTERPRETATION OF 500 MB DPVA 224. RAINBOW TIDBITS 225. WHY CAN IT BE VERY COLD ON A SUNNY DAY? 226. HOW CAN TEMPERATURES WARM ON A CLOUDY DAY? 227. INTERPRETATION OF AVERAGE HIGH AND LOW TEMPERATURE 228. WHY DOESN'T GRAVITY PUSH CLOUDS TO THE GROUND? 229. WHO IS A METEOROLOGIST? 230. CAN ICE MELT WHEN THE AIR TEMPERATURE IS SUB-FREEZING? 231. RANGE FOLDING AND THE DOPPLER DILEMMA 232. WHICH PRECIPITATION TYPES ARE BEST DETECTED BY RADAR? 233. WHAT HAPPENS DURING VELOCITY ALIASING / RANGE FOLDING 234. WHAT HAPPENS DURING DUCTING? 235. HOW DOES RADAR DETECT PRECIPITATION PARTICLES? 236. CAN RADAR DETECT A TORNADO? 237. RADAR CHARACTERISTICS OF SUPERCELLS 238. WHAT IS A HOOK ECHO? 239. WHAT IS THE RELEVANCE OF CLEAR AIR MODE? 240. RADAR RADIAL VELOCITY TYPES 241. WHAT IS THE DOPPLER SHIFT? 242. WHAT IS THE MEANING OF A TVS ICON? 243. WHAT IS BEAM SPREADING AND THE CONSEQUENCES? 244. WHY DO MID-LEVELS HAVE HIGHEST RADAR REFLECTIVITY? 245. WHAT IS SPECTRUM WIDTH? 246. ACCURACY AND PRECISION? 247. WHAT ARE ANOMALOUS PROPAGATION AND FALSE ECHOS? 248. WHAT IS ATTENUATION? 249. WHAT IS VIL (VERTICALLY INTEGRATED LIQUID)? 250. RANGE, AZIMUTH, ELEVATION ANGLE AND ECHO HEIGHT 251. VALUE OF THE WIND CHILL INDEX 252. WHAT IS A "WHITE CHRISTMAS"? 253. WHY AREN'T COLD FRONTS AND CAA LIFTING MECHANISMS? 254. SIMPLIFIED OMEGA EQUATION (THERMAL ADVECTION TERM) 255. SIMPLIFIED OMEGA EQUATION (VORTICITY ADVECTION TERM) 256. JET STREAK WIND AND JET STREAK MOVEMENT 257. WHAT IS THE CONVECTIVE TEMPERATURE? 258. MODIFICATION OF A STAGNANT AIR MASS 259. PRECIPITATION EFFECT ON WET-BULBING OUT PROCESS 260. WHY IS MOIST AIR LESS DENSE THAN DRY AIR AT SAME TEMP? 261. WHAT CAUSES GIANT SNOWFLAKES? 262. THUNDERSTORMS AND FIRE 263. AN EXAMPLE OF COLD THICKNESS BIASING 264. WHEN ARE CELSIUS AND FAHRENHEIT THE SAME? 265. WEATHER WISHES VERSUS WEATHER REALITY 266. PRECIPITATION PROBABILITY BRAIN TEASER 267. DIFFERENCES BETWEEN ANALYZING WAA AND ISENTROPIC LIFT 268. WHY ARE TEMPERATURES COOLER IN RURAL AREAS? 269. WHAT IS AN ISOTHERMAL LAYER? 270. IRRELEVANCE OF SFC RH FOR PRECIPITATION PREDICTION 271. 10 POPULAR WEBSITES FOR REALTIME U.S. WEATHER DATA 272. HOW TO DETECT AND FORECAST VIRGA 273. WHAT IS A BACK DOOR COLD FRONT? 274. WHAT IS HEAT LIGHTNING? 275. SHEAR AND THUNDERSTORM TYPE 276. WHAT CAUSES GREAT VISIBILITY? 277. FORECASTING HIGHS AND LOWS USING MOS 278. FORECASTING SURFACE HIGH USING 850-mb TEMP 279. WHY HUMID NIGHTS TEND TO BE WARMER THAN DRY NIGHTS 280. TV WEATHER: AMS AND NWA SEAL FAQ 281. THE TOP 5 REASONS POLAR AREAS ARE COLD 282. THE SANTA ANA WIND 283. HOW DOES WIND CREATE SOUND? 284. UNDERSTANDING POP (CHANCE OF PRECIPITATION) 285. WEATHER AND BASEBALL FLIGHT 286. LIGHTNING STORMS 287. STORMS THAT DO NOT HAVE A TORNADO 288. WHAT IS A DERECHO? 289. SEVERE STORM DEATHS 290. UNITS OF HELICITY AND CAPE 291. SKEW-T: A LOOK AT TP (TROPOPAUSE) 292. SKEW-T: A LOOK AT FRZ (FREEZING LEVEL) 293. SKEW-T: A LOOK AT WB0 (WET BULB ZERO LEVEL) 294. SKEW-T: A LOOK AT PW (PRECIPITABLE WATER) 295. SKEW-T: A LOOK AT RH (RELATIVE HUMIDITY) 296. SKEW-T: A LOOK AT MAXT (MAXIMUM TEMPERATURE) 297. SKEW-T: A LOOK AT TH (THICKNESS) 298. SKEW-T: A LOOK AT L57 (700 TO 500 MB LAPSE RATE) 299. SKEW-T: A LOOK AT LCL (LIFTED CONDENSATION LEVEL) 300. SKEW-T: A LOOK AT LI (LIFTED INDEX) 301. SKEW-T: A LOOK AT SI (SHOWALTER INDEX) 302. SKEW-T: A LOOK AT TT (TOTAL TOTALS) 303. SKEW-T: A LOOK AT KI (K INDEX) 304. SKEW-T: A LOOK AT SW (SWEAT INDEX) 305. SKEW-T: A LOOK AT CAPE (PURE INSTABILITY) 306. SKEW-T: A LOOK AT CINH (CONVECTIVE INHIBITION) 307. SKEW-T: A LOOK AT SBLCL (SURFACE BASED LCL) 308. SKEW-T: A LOOK AT CAP (CAPPING LAYER) 309. SKEW-T: A LOOK AT LFC (LEVEL OF FREE CONVECTION) 310. SKEW-T: A LOOK AT EL (EQUILIBRIUM LEVEL) 311. SKEW-T: A LOOK AT MPL (MAXIMUM PARCEL LEVEL) 312. SKEW-T: A LOOK AT STM (STORM MOTION) 313. SKEW-T: A LOOK AT HEL (HELICITY) 314. SKEW-T: A LOOK AT EHI (ENERGY HELICITY INDEX) 315. SKEW-T: A LOOK AT BRN (BULK RICHARDSON NUMBER) 316. SKEW-T: A LOOK AT SRDS (STORM RELATIVE DIR. SHEAR) 317. SKEW-T: A LOOK AT Tdd (DEWPOINT DEPRESSION) 318. SKEW-T: A LOOK AT MW (MAXIMUM WIND) 319. SKEW-T: A LOOK AT STORM UVV 320. SKEW-T: A LOOK AT CCL (CONVECTIVE CONDENSATION LEVEL) 321. SKEW-T: A LOOK AT TEI (THETA-E INDEX) 322. SKEW-T: A LOOK AT 0-3 KM SHEAR 323. SKEW-T: A LOOK AT SURFACE RH 324. SKEW-T: A LOOK AT THETA-E 325. SKEW-T: A LOOK AT EI (ENERGY INDEX) 326. WHY ARE HURRICANES HARD TO PREDICT? 327. WHAT IS THE POLAR VORTEX? 328. WHAT IS A UVV MAX? 329. WHAT IS A COLD AIR FUNNEL? 330. HOW IS DEWPOINT CALCULATED? 331. INSIDE RH AS A FUNCTION OF OUTSIDE WEATHER 332. THE "WHAT DAY IS IT OVERNIGHT?" PROBLEM 333. A BAROMETRIC PRESSURE TIDBIT AND A PERPLEXION 334. WHAT CAUSES THUNDERSNOW? 335. COLD AIR DAMMING EXAMPLE 336. DYNAMIC PRECIP vs. CONVECTIVE PRECIP 337. TEXAS DRYLINE PROPAGATION ON MODELS 338. POLAR JET STREAM VORTICES AND JET STREAKS 339. HORIZONTAL WIND SPEED AT THE CENTER OF A CLOSED LOW 340. REASONS FOR UNSTABLE LIFTED INDEX 341. WHAT IS A HEAT BURST? 342. AN ANALYSIS OF GIANT HAIL 343. LOCATING A FRONTAL BOUNDARY 344. INITIALIZING A MODEL 345. WHY ARE HOT AND HUMID DAYS OFTEN HAZY? 346. SNOW TO LIQUID EQUIVALENT 347. FROST POINT AND DEW POINT 348. WHAT IS DIFFERENTIAL ADVECTION? 349. RELATIONSHIP BETWEEN THICKNESS AND TEMP. GRADIENTS 350. LONGWAVE TROUGH MOVEMENT 351. SEVERE STORM STRUCTURE: ANVIL 352. SEVERE STORM STRUCTURE: OVERSHOOTING TOP 353. SEVERE STORM STRUCTURE: MAMMATUS 354. SEVERE STORM STRUCTURE: FLANKING LINE 355. SEVERE STORM STRUCTURE: RAIN CORE / HAIL CORE 356. SEVERE STORM STRUCTURE: WALL CLOUD 357. SEVERE STORM STRUCTURE: RAIN-FREE BASE 358. SEVERE STORM STRUCTURE: FLANK DOWN DRAFTS 359. WHAT IS DIFFERENCE BETWEEN ICE FOG AND FREEZING FOG? 360. WHAT IS DEEPENING AND FILLING OF A LOW? 361. DIFFERENCE BETWEEN ENHANCED-V AND V-NOTCH 362. WHAT IS AN INDIAN SUMMER? 363. WHAT IS A SHOWER? 364. WHAT IS A DRYLINE BULGE? 365. WHAT ARE THE DOG DAYS OF SUMMER? 366. BITTER COLD IN NORTHEAST U.S. 367. THE THERMAL LOW 368. TERMS FOR HEAVY RAIN 369. SOLAR INTENSITY AND SNOW SUBLIMATION 370. FREEZING RAIN EXAMPLE 371. FORECAST BUST: CLOUD COVER 372. FORECAST BUST: PRECIPITATION 373. FORECAST BUST: FRONTS 374. FORECAST BUST: SNOW COVER 375. FORECAST BUST: CAP 376. FORECAST BUST: WIND SPEED AND DIRECTION 377. FORECAST BUST: TIME 378. FORECAST BUST: SMALL SCALE INFLUENCES 379. FORECAST BUST: HUMAN ERROR 380. FORECAST BUST: UNCERTAINTY 381. REFLECTIVITY GRADIENT AND SEVERE WEATHER 382. WHAT ARE ECHO TOPS AND THEIR IMPORTANCE? 383. WHAT IS BRIGHT BANDING AND HOW DOES IT OCCUR? 384. VIL AND UPDRAFT STRENGTH 385. HOW DOES SNOW LOOK ON RADAR? 386. WHAT CREATES A BOW ECHO? 387. WHAT IS AN INFLOW NOTCH? 388. ANVIL BLOWOFF ON RADAR 389. RECOGNIZING FLOODING POTENTIAL ON RADAR 390. CALCULATION OF RADAR SHEAR 391. INVERSIONS AND RADAR GROUND CLUTTER 392. Rmax and Vmax AND THE PULSE REPETITION FREQUENCY 393. VEERING AND BACKING WIND ON RADIAL VELOCITY 394. WAVELENGTH AND FREQUENCY OF LIGHT AND PERSPECTIVE 395. INCREASING THE POWER RETURNED TO THE RADAR 396. RANGE FOLDING AND DETECTING RANGE FOLDED ECHOES 397. ECHO HEIGHT ERRORS DUE TO ABNORMAL REFRACTION 398. RADAR REFLECTIVITY PITFALLS 399. SEVERE STORM TRACKING TECHNIQUES 400. WHAT IS A PULSE STORM? 401. 50+ TIPS FOR IMPROVING AMS / NWA / RESUME TAPE 402. WHY ARE CERTAIN REGIONS OF A HURRICANE STRONGER? 403. WHY IS HAIL RARE IN A HURRICANE? 404. WHY ARE TORNADOES MORE COMMON IN THE PLAINS? 405. WHAT CREATES A CAP? 406. WHAT ARE STRAIGHT-LINE WINDS? 407. WHAT IS THE THERMAL WIND? 408. FROST POINT AND FORECAST IMPLICATIONS 409. THUNDERSTORMS AND 700 MB TEMPERATURE 410. AIR PRESSURE ON WEATHERCASTS 411. HABY'S TOP 5 PLACES TO LIVE TO OBSERVE WEATHER 412. EYEWALL REPLACEMENT CYCLE 413. RITA AND KATRINA: THE CAT 5 SISTERS 414. HOW IS THE CENTER OF A TROPICAL SYSTEM DETERMINED? 415. OVERUSED WORDS OR PHRASES IN BROADCASTING 416. HOW DOES A HURRICANE FORM? 417. HOW DOES A TORNADO FORM? 418. THE CASE OF TEMPS WARMING BEHIND A COLD FRONT 419. AMS CBM TEST: STUDY GUIDE 420. BOUNDARY LAYER DECOUPLING 421. FORECASTING: ADVECTION ALOFT AND SURFACE TEMPERATURE 422. FORECASTING: UPSTREAM CONDITIONS 423. FORECASTING: STRONG RADIATIONAL COOLING 424. FORECASTING: TIMING A FRONT 425. FORECASTING: OCEAN AND LAKE INFLUENCE 426. FORECASTING: BEWARE THE DARN CLOUDS 427. FORECASTING: DON'T FRET OVER LOW POP AND LOW QPF 428. FORECASTING: TIMING PRECIPITATION 429. FORECASTING: TAKING MODEL CONSENSUS 430. FORECASTING: SYNTHESIS 431. INTRODUCTION TO MODEL MOS 432. WIND DIRECTION AND WEATHER FORECASTING 433. THERMOMETER VARIABILITY 434. PRECIPITATION INTENSITY 435. FORECASTING ADVECTION FOG 436. IN THE BEAR'S CAGE 437. CORE PUNCHING THE LION'S DEN 438. HEATING AND COOLING DEGREE DAYS 439. LIGHT WIND AND THE TEMPERATURE FORECAST 440. WRAP-AROUND SNOW 441. HABY'S HURRICANE PREPARATION ADVICE 442. HABY'S ICE STORM PREPARATION ADVICE 443. HABY'S LIGHTNING AND FLOODING PREPARATION ADVICE 444. DENSITY OF AIR 445. NEGATIVE TEMPERATURE AND DEWPOINT 446. 11 LESSER TALKED ABOUT DRIVING WEATHER PROBLEMS 447. OROGRAPHIC LIFTING 448. CYCLONIC AND ANTICYCLONIC SPIN 449. WHAT CREATES LOWER PRESSURE? 450. WHAT IS A WEATHER PATTERN? 451. DOES GLOBAL WARMING PRODUCE STRONGER HURRICANES? 452. SURFACE TEMPERATURE AND PRECIPITATION TYPE 453. WHY IS ITCZ MEAN POSITION NORTH OF THE EQUATOR? 454. DIFFERENCE BETWEEN WEATHER AND CLIMATE 455. WHAT IS DRY AIR? 456. ADIABATIC TEMPERATURE AND DEWPOINT CHANGES 457. WHAT IS A TROUGH AND A RIDGE? 458. WHAT IS AN AIR MASS THUNDERSTORM? 459. WHAT THERMAL ADVECTION IS NOT 460. FINDING THE L OR H BY SURFACE WIND DIRECTION 461. HOW MUCH FASTER IS LIGHTNING THAN THUNDER? 462. WHAT IS CIFK AND CISK? 463. WATER AND REFLECTION OF LIGHT 464. WHAT IS A CHINOOK? 465. GETTING SEVERE WEATHER INFORMATION 466. ACTIVE AND INACTIVE FRONTS 467. WHY IS EARTH A BALL SHAPE? 468. HOW DOES FREEZING RELEASE HEAT ENERGY? 469. TOP 10 WEATHER RELATED PROBLEMS PEOPLE COMPLAIN ABOUT 470. RATE OF EVAPORATION 471. WHAT IF?: EARTH WAS NOT TILTED 472. WHAT IF?: EARTH DID NOT ROTATE 473. WHAT IF?: EARTH WAS TILTED BY 90 DEGREES 474. CONVERTING MILLIBARS TO INCHES OF MERCURY 475. WHAT IS THE PRESSURE GRADIENT FORCE? 476. WHAT IS FRICTION? 477. WHAT IS SPECIFIC VOLUME? 478. TWICE AS WARM RIDDLE 479. WIND POWER RIDDLE 480. TEMPERATURE CONVERSION RIDDLE 481. RUM BAROMETER RIDDLE 482. DENSITY COMPARISON RIDDLE 483. Z TIME RIDDLE 484. HELIUM BALLOON RIDDLE 485. RELATIVE HUMIDITY RIDDLE 486. STORM ENERGY RIDDLE 487. MASS OF ATMOSPHERE RIDDLE 488. NUMBER OF RAINDROPS RIDDLE 489. GROWING CLOUD RIDDLE 490. STORM DEATHS 491. WORLD WEATHER RECORDS 492. U.S. WEATHER RECORDS 493. TOP 10 BEST JOBS IN METEOROLOGY 494. OPTIMUM CONDITIONS FOR RECORD HIGH OR LOW TEMP 495. A BETTER USE OF TERMS IN BROADCAST METEOROLOGY 496. NORTH ATLANTIC OSCILLATION 497. SOUTHERN OSCILLATION INDEX 498. ARCTIC OSCILLATION 499. WHO IS TO BLAME FOR KATRINA NEW ORLEANS DISASTER? 500. 500th HABY HINT MILESTONE REACHED 501. ASSUMPTIONS OF ADIABATIC PROCESS 502. CHANGES IN THERMO VARIABLES AS A PARCEL RISES 503. MORNING CAP AND THUNDERSTORMS 504. HOW DOES DRY AIR ALOFT MAKE STORMS MORE SEVERE? 505. WHAT ARE KISSING JETS? 506. MORNING SOUNDING AND SEVERE WEATHER 507. IMPORTANCE OF SHOWING JET STREAM MAP 508. THE LAYERS OF THE ATMOSPHERE 509. MEASURING AND VERIFICATION OF PRECIPITATION 510. RELATIVE HUMIDITY IN THE HOME 511. OPTICAL DEPTH OF CLOUDS 512. CLOUD DETECTION (IR vs. VIS) 513. SURFACE FEATURES (IR & VIS) 514. STABLE VS. UNSTABLE CLOUDS 515. FLOW AROUND THE BURBUDA HIGH INTO THE USA 516. SATELLITE PITFALLS 517. RESOLUTION, BRIGHTNESS, CONTRAST 518. SAT: DETERMINING CLOUD HEIGHT AND TYPE 519. GOES SATELLITES IN USE 520. SATELLITE OBSERVATION OF CLOUDS 521. EMITTED RADIATION AND WAVELENGTH OF MAX EMISSION 522. CALCULATING SUN ANGLE 523. HOW DOES WATER VAPOR IMAGERY WORK? 524. THE 6 CHANGES OF STATE OF WATER 525. LAND BREEZES OFTEN WEAKER THAN SEA BREEZES 526. WHY DOES TEMP. DECREASE WITH HEIGHT IN TROPOSPHERE? 527. HOW DOES FOG MIX OUT? 528. ANVIL EXPANSION RATE 529. POES vs. GOES 530. FRONTAL TRIPLE POINT 531. THE MCC (MESOSCALE CONVECTIVE COMPLEX) 532. WATER AND SOLAR REFLECTION / ABSORPTION 533. HEAT DISTRIBUTION IN THE TROPOSPHERE 534. SNOW COVER AND RADIATION BUDGET 535. POWERFUL LIFTING MECHANISMS 536. FACTORS INFLUENCING THUNDERSTORM HEIGHT 537. DUST ON SATELLITE 538. RADIATION IN THE ATMOSPHERE 539. CUMULUS VS. STRATUS 540. SATELLITE SOUNDER DATA 541. THE PERFECT TORNADIC ENVIRONMENT 542. REPEATING OF WEATHER (WEATHER PATTERN) 543. METEOROLOGY: EDUCATION, JOBS, CAREERS 544. HAIL SIZE AND HAIL DAMAGE 545. FOG DISSIPATION 546. COLD FRONT CROSS SECTION 547. RAINDROPS AND STARS 548. RETROGRADING LOW 549. FIRE WEATHER 550. “AVERAGE” RAINFALL, WEATHER AND CLIMATE 551. RECORD TEMPERATURES AND TIME OF DAY 552. REASONS FOR RECORD TEMPERATURES 553. WHY ARE DESERTS HOT? 554. CREATION OF GREAT PLAINS THUNDERSTORM CAP (EML) 555. INFLUENCE OF TOPOGRAPHY ON WEATHER 556. THE CUMULUS CONGESTUS LOOK 557. FACTORS PRODUCING SEVERE CONVECTIVE WIND GUSTS 558. DEALING WITH NEGATIVE INTEGERS 559. WHAT DETERMINES CLOUD BASES? 560. HOW DOES A STRAW WORK? 561. GENERATION OF A TUBE OF LOW LEVEL VORTICITY 562. COMPARISON OF VERY DRY AND VERY MOIST AIR 563. DECIMAL PLACES WITHIN TEMPERATURES 564. RELATIVE HUMIDITY PITFALLS 565. WHAT MAKES AIR MASSES MOVE? 566. GASES OF THE DRY TROPOSPERE 567. HABYTIME MINI LECTURE 1: WIND 568. HABYTIME MINI LECTURE 2: COLD AIR ADVECTION 569. HABYTIME MINI LECTURE 3: WARM AIR ADVECTION 570. HABYTIME MINI LECTURE 4: COLD FRONT 571. HABYTIME MINI LECTURE 5: THE WARM FRONT 572. HABYTIME MINI LECTURE 6: THE DRY LINE 573. HABYTIME MINI LECTURE 7: TROUGHS 574. HABYTIME MINI LECTURE 8: RIDGES 575. HABYTIME MINI LECTURE 9: POSITIVE VORTICITY ADVECTION 576. HABYTIME MINI LECTURE 10: NEGATIVE VORTICITY ADVECTION 577. HABYTIME MINI LECTURE 11: CREATION OF THE JET STREAM 578. HABYTIME MINI LECTURE 12: MID-LATITUDE CYCLONE 579. HABYTIME MINI LECTURE 13: THE INVERSION 580. HABYTIME MINI LECTURE 14: DEWPOINT AND HUMIDITY 581. HABYTIME MINI LECTURE 15: PRECIPITATION 582. HABYTIME MINI LECTURE 16: SEVERE WEATHER BIG 4 583. HABYTIME MINI LECTURE 17: CONVECTIVE INSTABILITY 584. HABYTIME MINI LECTURE 18: CONVECTIVE WIND GUSTS 585. HABYTIME MINI LECTURE 19: HAIL 586. HABYTIME MINI LECTURE 20: SIGNIFICANT TORNADOES 587. HABYTIME MINI LECTURE 21: SIGNIFICANT HURRICANES 588. HABYTIME MINI LECTURE 22: SNOW 589. HABYTIME MINI LECTURE 23: SLEET 590. HABYTIME MINI LECTURE 24: FREEZING RAIN 591. REASONS WHY MOIST AIR SEEMS DENSER 592. THE FORCE OF THE AIR 593. A DESERT NEXT TO THE OCEAN 594. COLONIZING MARS 595. HABYTIME MINI LECTURE 25: POLAR JET (WINTER VS. SUMMER) 596. WARM FRONT DIFFERENTIAL ADVECTION 597. COLD FRONT DIFFERENTIAL ADVECTION 598. OCCLUDED FRONT DIFFERENTIAL ADVECTION 599. NIMBOSTRATUS AND CUMULONIMBUS 600. WILL FORECASTS ALWAYS BE PROBABILITY FORECASTS? 601. HABYTIME MINI LECTURE 26: QUADRANTING A JET STREAK 602. WEATHER AND FOOTBALL 603. SNOW FORECAST AND TEMPERATURE FORECAST 604. WEATHER AND BASEBALL 605. EASIER TO MEASURE AND FORECAST: RAIN OR SNOW? 606. WEATHER AND GOLF 607. LAYERS OF THE ATMOSPHERE 608. HABYTIME MINI LECTURE 27: THE MILANKOVITCH CYCLES 609. WHAT IS A MONSOON? 610. MORNING WARMING 611. HABYTIME MINI LECTURE 28: HYDROSTATIC BALANCE 612. HABYTIME MINI LECTURE 29: COLD VS. WARM CORE HIGH 613. HABYTIME MINI LECTURE 30: WARM CORE LOWS 614. HABYTIME MINI LECTURE 31: UPSLOPE AND DOWNSLOPE FLOW 615. HABYTIME MINI LECTURE 32: SURFACE SOLAR INTENSITY 1 616. HABYTIME MINI LECTURE 33: HYPSOMETRIC EQUATION 617. HABYTIME MINI LECTURE 34: (IR)REVERSIBLE ADIABATIC 618. TIME ZONES AND SAVINGS TIME 619. HABYTIME MINI LECTURE 35: WET BULBING 620. HABYTIME MINI LECTURE 36: BERGERON PROCESS 621. HABYTIME MINI LECTURE 37: VIRTUAL TEMPERATURE 622. SCIENTIFIC METHOD 623. HABYTIME MINI LECTURE 38: LCL AND CCL 624. HABYTIME MINI LECTURE 39: ELEVATED CONVECTION 625. HABYTIME MINI LECTURE 40: CONDITIONAL INSTABILITY 626. HABYTIME MINI LECTURE 41: TROPOPAUSE (TROP) 627. HABYTIME MINI LECTURE 42: SUBSIDENCE INVERSION 628. HABYTIME MINI LECTURE 43: SPEED AND DIR. WIND SHEAR 629. HABYTIME MINI LECTURE 44: THE HODOGRAPH 630. HABYTIME MINI LECTURE 45: STORM RELATIVE WIND 631. HABYTIME MINI LECTURE 46: HORIZONTAL VORTICITY 632. HABYTIME MINI LECTURE 47: 0 to 3 KM CAPE AND TORNADOES 633. HABYTIME MINI LECTURE 48: HELICITY 634. HABYTIME MINI LECTURE 49: MOST UNSTABLE CAPE 635. HABYTIME MINI LECTURE 50: MEAN LAYER CAPE 636. HABYTIME MINI LECTURE 51: OVERWEIGHT CAPE 637. DISTINCTION BETWEEN POLAR AND ARCTIC AIR 638. HABYTIME MINI LECTURE 52: 1000 to 700 MB THICKNESS 639. LIGHT SNOW IN VERY COLD AIR 640. HABYTIME MINI LECTURE 53: ICE PELLETS (SLEET) 641. HABYTIME MINI LECTURE 54: FREEZING RAIN 642. HABYTIME MINI LECTURE 55: HURRICANE AND SHORE POSITION 643. HABYTIME MINI LECTURE 56: RAIN SHADOW EFFECT 644. TERMINAL VELOCITY 645. HABYTIME MINI LECTURE 57: MOUNTAIN WAVE CLOUDS 646. CLAUSIUS-CLAPEYRON EQUATION 647. TORNADO VS. FUNNEL 648. TORNADO VS. WATERSPOUT 649. HABYTIME MINI LECTURE 58: COMMON CURRENT CONDITIONS 650. WET VS. DRY SNOW 651. HABYTIME MINI LECTURE 59: SURFACE AIR PRESSURE 652. HABYTIME MINI LECTURE 60: METR. EQUATION TERMS 653. THE WATER CYCLE 654. GEOLOGIC CLIMATE CHANGE 655. EVAPORATION AND PRECIPITATION DEVELOPMENT 656. HABYTIME MINI LECTURE 61: MOVEMENT VOCABULARY 657. OZONE SHIELD 658. PHOTOSYNTHESIS 659. HABYTIME MINI LECTURE 62: FLOODING FACTORS 660. HABYTIME MINI LECTURE 63: TROPICAL CYCLONE DEFLECTION 1 661. BACK DOOR COLD FRONT 662. HABYTIME MINI LECTURE 64: HAIL STREAK 663. KELVIN-HELMHOLTZ WAVES 664. HABYTIME MINI LECTURE 65: CONTOUR LINES 665. HABYTIME MINI LECTURE 66: THE POLAR VORTEX 666. LATITUDE AND LONGITUDE 667. CLIMATE ZONES 668. THUNDERSTORM GLACIATION 669. HABYTIME MINI LECTURE 67: SPEED AND DIRECTIONAL SHEAR 670. HABYTIME MINI LECTURE 68: SLIM CAPE AT START 671. LENTICULAR CLOUDS 672. HABYTIME MINI LECTURE 69: PREP FOR UNIVERSITY METR. 673. HABYTIME MINI LECTURE 70: REASON FOR SEASONS 674. CALCULATING WEIGHTED AVERAGE 675. HABYTIME MINI LECTURE 71: EQUATION OF STATE 676. HABYTIME MINI LECTURE 72: WHEN LIGHT STRIKES 677. HABYTIME MINI LECTURE 73: THUNDERSTORM FACTORS 678. HABYTIME MINI LECTURE 74: SURFACE SOLAR INTENSITY 2 679. HABYTIME MINI LECTURE 75: HELICITY WITH CAPE 680. INTERPOLATION 681. BOYLE’S LAW AND CHARLES’ LAW 682. SATURATION VAPOR PRESSURE 683. WARMER AIR AND MORE MOISTURE 684. PRESSURE WITH ALTITUDE 685. DAYLENGTH VARIATION 686. MOUNTAIN WAVE TURBULENCE 687. CONDENSATION AND DEPOSITION NUCLEI 688. PRESSURE AND TEMPERATURE RELATIONSHIP 689. ARCHIMEDES’ PRINCIPLE 690. COLUMN AVERAGE RELATIVE HUMIDITY 691. DIRECTION OF HEAT FLOW 692. TROPICAL STORM AND TROUGH INFLUENCE 693. PRECIPITATION UNDER THE RADAR 694. HABYTIME MINI LECTURE 76: SURFACE SOLAR INTENSITY 3 695. NEWTON’S LAWS 696. LOW LEVEL JET 697. THERMAL ADVECTION AND HEIGHT CHANGE 698. PRESSURE TROUGHS 699. HABYTIME MINI LECTURE 77: INSTABILITY VS. LIFT 700. HABYTIME MINI LECTURE 78: OPTIMUM SNOWFALL REGION 701. THETA-E INCREASE 702. LES: FRICTIONAL CONVERGENCE 703. CAP AND BASKETBALL ANALOGY 704. COMPARE AND CONTRAST: MID-LAT CYCLONE AND HURRICANE 705. COLD OCCLUSION 706. SFC WARMING- SENSIBLE VS. LATENT HEAT 707. ATMOSPHERIC GREENHOUSE EFFECT 708. HEAT SHIELD VS. BLANKET 709. PRECIPITATION RESISTANCE 710. DOWNBURST VS. TORNADO DAMAGE 711. TOPOGRAPHIC CONVERGENCE 712. RIGHT HAND TWIST MODEL 713. VALLEY WEATHER 714. TORNADO NAMES 715. TORNADO OBSTRUCTIONS 716. AMPLIFIED STORM SURGE 717. CONDUCTION, CONVECTION, RADIATION 718. THUNDERSTORM TILTING 719. THE DOWNDRAFT 720. RADIATIONAL COOLING INVERSION 721. FALSE TORNADOES 722. LOWERED CLOUD BASE 723. ALBERTA CLIPPER 724. CHINOOK WIND 725. HABYTIME MINI LECTURE 79: CONVECTIVE EROSION OF CAP 726. COLD AIR DAMMING 727. URBAN HEAT ISLAND 728. MARINE LAYER 729. ELEVATED THUNDERSTORM 730. WINDY WEATHER 731. BAROCLINIC LEAF 732. SUBTROPICAL JET 733. SCALES OF MOTION 734. ELEVATED WARM LAYER EROSION 735. LAPSE RATES 736. DRY MICROBURST 737. BOUNDARY LAYER DECOUPLING 738. TRAPPING LAYERS 739. TURBULENCE 740. BELOW GROUND WEATHER 741. THE GEOSTROPHIC WIND 742. THE SURFACE WIND 743. THE GRADIENT WIND 744. SUBGEOSTROPHIC AND SUPERGEOSTROPHIC WIND 745. THE CYCLOSTROPHIC WIND 746. HABYTIME MINI LECTURE 80: METEOROLOGICAL WINDS 747. AIR DENSITY DIFFERENCES 748. 2 METHODS OF QUADRANTING JET STREAK 749. WIND SPEED INCREASING WITH HEIGHT 750. BLACK ICE 751. GLOBAL TEMPERATURE CHANGE 752. HABYTIME MINI LECTURE 81: CLIMATE CHANGE 753. POSITIVE AND NEGATIVE FEEDBACK 754. SOURCES OF ENERGY 755. OCEAN CHANGES WHEN CLIMATE TEMPERATURE WARMS 756. GRADUAL CHANGE VS. TIPPING POINT CLIMATE CHANGE 757. SEA LEVEL CHANGE 758. CLOUD ALBEDO EFFECT 759. EVIDENCE OF PAST CLIMATE 760. ICE ALBEDO EFFECT 761. INTRO BROADCAST METEOROLOGY 762. BROADCAST METEOROLOGY SKILLS 763. BROADCAST METEOROLOGY EDUCATION 764. BROADCAST METEOROLOGY INFLUENCE 765. BROADCAST METEOROLOGY WORKPLACE 766. BROADCAST METEOROLOGY CAREER PATH 767. BROADCAST METEOROLOGY CHALLENGES 768. BROADCAST METEOROLOGY VIEWER WANTS 769. BROADCAST METEOROLOGY REWARDS 770. BROADCAST METEOROLOGY FUTURE 771. PERCENTAGES IN METEOROLOGY 772. LONG TERM FORECASTS 773. RELATIVE HUMIDITY 774. RECORD LOW MAXIMUM AND HIGH MINIMUM 775. THE MEANING OF “STORM” 776. VISIBILITY 777. SEVERE STORM MOVEMENT AND DEVELOPMENT 778. WINTER CLOUDS IN MID LATITUDES 779. WINTER DRIVING HAZARDS 780. WHY A FORECAST IS WRONG 781. WX CHANGERS- FRONTS 782. WX CHANGERS- CHINOOK AND UPSLOPE EVENTS 783. WX CHANGERS- SHALLOW INVERSION 784. WX CHANGERS- SUNSHINE 785. WX CHANGERS- DOWNDRAFT 786. WX CHANGERS- EVAPORATIVE COOLING 787. WX CHANGERS- CAP BREAK 788. WX CHANGERS- MARINE LAYER 789. WX CHANGERS- PASSAGE OF 32 F LINE 790. WX CHANGERS- DENSE FOG 791. WX CHANGERS- LAKE-EFFECT SNOW 792. WX CHANGERS- HEAT BURST 793. WX CHANGERS- NOR’EASTERS 794. WX CHANGERS- HABOOB 795. WX CHANGERS- DRYLINE 796. WX CHANGERS- HURRICANE EYE 797. WX CHANGERS- SUPERCELL 798. WX CHANGERS- SEA BREEZE 799. WX CHANGERS- MID-LATITUDE CYLONE 800. WX CHANGERS- FLASH FLOODING 801. HOME ENVIRONMENT: HUMIDITY 802. HOME ENVIRONMENT: TEMPERATURE 803. HOME ENVIRONMENT: COOLING SOURCES 804. HOME ENVIRONMENT: SUN 805. HOME ENVIRONMENT: WX PROOFING 806. NOR’EASTER: LOW LEVELS 807. NOR’EASTER: UPPER LEVELS 808. THE SEVERE WEATHER AND STORM FACTOR 809. ATMOSPHERIC RIVER 810. ABNORMAL WEATHER 811. CROP FREEZING DANGERS 812. WX MODEL 1: U.S. West Coast Storm 813. WX MODEL 2: Clipper System 814. WX MODEL 3: Cold Air Plunge 815. WX MODEL 4: Cut-off Low 816. WX MODEL 5: Rex Block 817. WX MODEL 6: Cold Air Advection 818. WX MODEL 7: CAA sinking 819. WX MODEL 8: Bombogenesis 820. WX MODEL 9: Cold Air Progression 821. WX MODEL 10: Model Convergence 822. WX MODEL 11: Wave on Cold Front 823. WX MODEL 12: UVV Max 824. WX MODEL 13: Meridional Flow 825. WX MODEL 14: Cold Core High 826. WX MODEL 15: Low Level Moisture 827. WX MODEL 16: Cold Air Retreat 828. WX MODEL 17: Shortwave 829. WX MODEL 18: The Ridge 830. WX MODEL 19: Return Flow 831. WX MODEL 20: Temp Gradient and Jet Stream 832. WX MODEL 21: Upslope Flow with Low Pressure 833. WX MODEL 22: Sideways Trough 834. WX MODEL 23: Polar High 835. WX MODEL 24: Vorticity Generation 836. WX MODEL 25: Circulation and Convergence 837. WX AND BIZ: UTILITIES 838. WX AND BIZ: SHOPPING 839. WX AND BIZ: PARK AND REC 840. WX AND BIZ: AGRICULTURE 841. BURST POINT SERIES: Temperature Convergence 842. BURST POINT SERIES: Moisture Convergence 843. BURST POINT SERIES: Outflow Convergence 844. BURST POINT SERIES: Frictional Convergence 845. BURST POINT SERIES: Solar Heating Max 846. BURST POINT SERIES: Natural Conv. Boundaries 847. BURST POINT SERIES: UVV Max 848. BURST POINT SERIES: Man-made Boundaries 849. BURST POINT SERIES: Old Boundaries 850. BURST POINT SERIES: Instability Max 851. BACKYARD METEOROLOGY: TEMPERATURE 852. BACKYARD METEOROLOGY: MOISTURE 853. BACKYARD METEOROLOGY: INSTABILITY 854. BACKYARD METEOROLOGY: INSTABILITY RELEASE 855. BACKYARD METEOROLOGY: WIND SHEAR 856. BACKYARD METEOROLOGY: FROPA 857. BACKYARD METEOROLOGY: LATENT HEAT 858. BACKYARD METEOROLOGY: PRECIPITATION TYPE 859. BACKYARD METEOROLOGY: PRECIPITATION RATE 860. BACKYARD METEOROLOGY: VARIOUS SIGHTS 861. POP and SNOWFALL FORECAST 862. WIND GUSTINESS OBSERVATIONS 863. WEATHER GIFT IDEAS 864. WINTER WEATHER BUSTS 865. BUTTERFLY EFFECT 866. SECLUDED METEOROLOGY: MIDDLE OF OCEAN 867. SECLUDED METEOROLOGY: POLAR REGIONS 868. SECLUDED METEOROLOGY: VERY HIGH ELEVATION 869. SECLUDED METEOROLOGY: MIDDLE OF HOT DESERT 870. SECLUDED METEOROLOGY: RAINFOREST 871. URBAN WX SERIES: TEMPERATURE 872. URBAN WX SERIES: AIR QUALITY 873. URBAN WX SERIES: MESOSCALE INFLUENCES 874. URBAN WX SERIES: STORM DAMAGE 875. URBAN WX SERIES: WEATHER PREP & MAINTENANCE 876. CLOUD SERIES: STRATUS 877. CLOUD SERIES: CUMULUS 878. CLOUD SERIES: CIRRUS 879. CLOUD SERIES: NO CLOUDS 880. CLOUD SERIES: COMPOSITE/NAMING/UNIQUE CLOUDS 881. WX & MOOD SERIES: HAPPY 882. WX & MOOD SERIES: GLOOMY 883. WX & MOOD SERIES: ON EDGE 884. WX & MOOD SERIES: HOPEFUL 885. WX & MOOD SERIES: FRUSTRATION 886. LOCAL FREAKISH WX SERIES: EXTREME HAIL 887. LOCAL FREAKISH WX SERIES: TORNADO 888. LOCAL FREAKISH WX SERIES: 4+ INCHES OF RAIN IN AN HOUR 889. LOCAL FREAKISH WX SERIES: 6+ INCHES OF SNOW IN AN HOUR 890. LOCAL FREAKISH WX SERIES: 3+ INCHES OF GRAUPEL 891. LOCAL FREAKISH WX SERIES: LIGHTNING STORM 892. LOCAL FREAKISH WX SERIES: 2+ INCHES SLEET STORM 893. LOCAL FREAKISH WX SERIES: WHAT THE HECK? 894. LOCAL FREAKISH WX SERIES: ZERO VISIBILITY FOG 895. LOCAL FREAKISH WX SERIES: HEAVY FREEZING RAIN 896. WHAT IS AN ISOBAR? 897. WHAT IS THE TEMP AND DEWPOINT? 898. HOW IS WIND DIRECTION DISPLAYED IN METEOROLOGY? 899. WHAT IS PRECIPITABLE WATER? 900. ISOBAR SPACING 901. RADAR MONITORING 902. WIND AND ISOBARS 903. CONVECTIVE SYSTEMS 904. DEWPOINT DEPRESSION 905. CAPE AND CONVECTIVE INHIBITION 906. STORM INFLUENCE ON SURFACE WIND 907. FLORIDA SEA BREEZE 908. DEVELOPING LOW PRESSURE 909. AIR PRESSURE 910. CLOUD COVER 911. HARD TO FORECAST: SPECIFICS (TIME AND PLACE) 912. HARD TO FORECAST: HURRICANE LANDFALL 913. HARD TO FORECAST: WINTER WEATHER IN THE SOUTH 914. HARD TO FORECAST: LOCAL VARIATION 915. HARD TO FORECAST: SNOW ACCUMULATION 916. HARD TO FORECAST: FOG 917. HARD TO FORECAST: TORNADOES 918. HARD TO FORECAST: 6 DAYS OUT AND BEYOND 919. HARD TO FORECAST: MEETING PUBLIC EXPECTATIONS 920. HARD TO FORECAST: STORM EVENT LOCATION 921. POST ANALYSIS: INTRO 922. POST ANALYSIS: LEARNING FROM MISTAKES 923. POST ANALYSIS: WEATHER PATTERNS REPEAT 924. POST ANALYSIS: EVENTS TO POST ANALYZE 925. POST ANALYSIS: THE PAYOFF 926. GEN T-STORM HAZARDS: LIGHTNING 927. GEN T-STORM HAZARDS: VIS, SLICK ROADS 928. GEN T-STORM HAZARDS: ROOF DAMAGE 929. GEN T-STORM HAZARDS: WIND 930. GEN T-STORM HAZARDS: WATER DAMAGE 931. AIR COMPOSITION: OXYGEN 932. AIR COMPOSITION: WATER VAPOR 933. AIR COMPOSITION: ARGON 934. AIR COMPOSITION: NITROGEN 935. AIR COMPOSITION: CARBON DIOXIDE 936. WX AND TIME OF DAY: MORNING DAYLIGHT 937. WX AND TIME OF DAY: AFTERNOON 938. WX AND TIME OF DAY: EVENING 939. WX AND TIME OF DAY: EARLY NIGHT 940. WX AND TIME OF DAY: LATE NIGHT 941. GRAPHICAL AREA DISPLAY: CAPE 942. GRAPHICAL AREA DISPLAY: CAPE CHANGE 943. GRAPHICAL AREA DISPLAY: MU (MOST UNSTABLE) CAPE 944. GRAPHICAL AREA DISPLAY: DD (DOWN DRAFT) CAPE 945. GRAPHICAL AREA DISPLAY: LI (LIFTED INDEX) 946. GRAPHICAL AREA DISPLAY: 850 to 500 mb LAPSE RATE 947. GRAPHICAL AREA DISPLAY: K INDEX 948. GRAPHICAL AREA DISPLAY: LCL 949. GRAPHICAL AREA DISPLAY: LFC (LEVEL OF FREE CONVECTION) 950. GRAPHICAL AREA DISPLAY: RH BETWEEN LCL and LFC 951. KNOWING WHERE A FRONT WILL MOVE 952. WHAT IS A MIXED LAYER AND ATMOSPHERIC MIXING? 953. WHAT IS A PARCEL? 954. WHERE DOES ISENTROPIC LIFTING OCCUR? 955. WHAT IS ADIABATIC THEORY? 956. LOCATING A FRONT ON A SOUNDING 957. HOW DOES DYNAMIC LIFT COMPARE TO CONVECTIVE LIFT? 958. WHAT IS LINEAR FORCING? 959. HOW ARE STORMS STEERED? 960. WHAT IS ATMOSPHERIC FORCING? 961. CLOUD DEVELOPMENT AND EXISTENCE ALOFT 962. CONVECTIVE DEVELOPMENT 963. WIND GUSTS 964. MOISTURE DEPTH AND STORMS 965. FROST/FREEZE ADVISORY 966. PRECIPITATION CHANCE 967. WEATHER, LOCATION AND INFLUENCE ON SEA LEVEL 968. LIMITING FACTORS FOR CONVECTION 969. DOES WIND MAKE THE TEMPERATURE COLDER? 970. HOW HIGH CAN STRONG STORM UPDRAFTS REACH? 971. WHERE IS THE TOP OF THE ATMOSPHERE? 972. SITUATIONS IN WHICH WIND CAN WARM THE WEATHER 973. WHAT IS STABILITY? 974. EAR POPPING 975. WHY DOES THE MOON HAVE BASICALLY NO ATMOSPHERE? 976. HOW MANY MOLECULES OF AIR ARE IN THE ATMOSPHERE? 977. WHAT CAUSES THE CONDENSATION ON A GLASS OF ICE WATER? 978. DIFFERENT FROM NORMAL 979. WHICH MONTH OF THE YEAR IS TYPICALLY WARMEST? 980. WHICH MONTHS OF THE YEAR ARE TYPICALLY COLDEST? 981. HOW DOES A NIGHTTIME RAIN IMPACT WEATHER? 982. FACTORS THAT INCREASE SUNBURN POTENTIAL 983. HOW DOES THE OCEAN INFLUENCE THE WEATHER? 984. WHAT ARE THE DIFFERENT TYPES OF LIGHTNING STRIKES? 985. REASONS FOR A WEATHER FORECAST 986. THE WORD “METEOROLOGY” 987. A “FLY IN THE OINTMENT” WHEN FORECASTING 988. WHAT IS “GROUND CLUTTER”? 989. WEATHER HOMONYMS 990. RAIN CHARACTERISTICS AND FLOODING 991. WHAT IS A MIXED BAG OF WINTER PRECIPITATION? 992. AVERAGE, MEAN, NORMAL 993. RADIATIONAL COOLING AND OVERNIGHT LOW TEMPERATURE 994. OVERNIGHT RADIATIONAL COOLING FACTORS 995. DEFINING FLOOD RISK 996. WHAT IS A TRIGGER MECHANISM? 997. WHAT IS MEANT BY “WASHES OUT”? 998. SEVERE WEATHER LOCATIONS 999. ICE FOG AND FREEZING FOG 1000. FUTURE OF WEATHER PREDICTION 1001. HOW ARE TROPOSPHERE LAYERS DIVIDED FOR WX ANALYSIS? Enter your search terms Submit search form   Web www.theweatherprediction.com SEARCH THIS SITE OR THE ENTIRE WEB WITH GOOGLE