Seed Words for SLäHILöS UOJA SIGIME
šPADE 'Jä'šTáTKUA ZáPAJú SLOVA LISTä OLELESSAH NIINEI' SUOJVOJE EHDOT RAKKAUS TäMä ARTIKKELI KäSITTELEE TUNNETTA SANAN MUISTA MERKITYKSISTä KATSO TäSMENNYSSIVU SYDäN LäNSIMAISESSA KULTTUURISSA RAKKAUDEN SYMBOLI FORD MADOX BROWN ROMEO JULIA RAKKAUS SYVä KIINTYMYKSEN TUNNE JOHONKIN USEIMMITEN TOISEEN HENKILööN KAHDEN IHMISEN VäLINEN MOLEMMINPUOLINEN RAKKAUS JOHTAA USEIN PARISUHTEESEEN RAKKAUTEEN SEKSUAALISUUTEEN PERUSTUVAAN KAHDENVäLISEEN SUHTEESEEN SISäLLYSLUETTELO PIILOTA MääRITELMIä LUOKITTELUJA BIOLOGIA USKONNOLLISIA KäSITYKSIä RAKKAUDESTA KRISTINUSKO ISLAM ISHQ JUMALAISEN RAKKAUDEN KäSITE KATSO MYöS LäHTEET KIRJALLISUUTTA AIHEESTA MUUALLA MääRITELMIä LUOKITTELUJA MUOKKAA MUOKKAA WIKITEKSTIä LäNSIMAISESSA KULTTUURISSA RAKKAUS JAETAAN USEIN PLATONIN ESITTELEMäN KOLMIJAON MUKAAN EROS EROOTTINEN RAKKAUS FILIA VELJELLINEN RAKKAUS AGAPE JUMALALLINEN RAKKAUS NELJäNTENä RAKKAUDEN MUOTONA VOIDAAN MAINITA AMOR ROMANTTINEN RAKKAUS BIOLOGIA MUOKKAA MUOKKAA WIKITEKSTIä TUTKIMUSTEN MUKAAN KUMPPANIN TUOKSU VAIKUTTAA PARINVALINTAAN IHMISET RAKASTUVAT TIETYNLAISEN FEROMONITUOKSUN OMAAVAAN IHMISEEN USKONNOLLISIA KäSITYKSIä RAKKAUDESTA MUOKKAA MUOKKAA WIKITEKSTIä KRISTINUSKO MUOKKAA MUOKKAA WIKITEKSTIä KRISTINUSKON MUKAAN RAKKAUS USKON TäRKEIN PERUSTA MATTEUKSEN EVANKELIUMIN MARKUKSEN EVANKELIUMIN MUKAAN JEESUS OPETTI RAKKAUDEN KAKSOISKäSKYN KäSKYSSä KEHOTETAAN RAKASTAMAAN JUMALAA KAIKESTA SYDäMESTä KAIKESTA MIELESTä KAIKESTA HENGESTä LäHIMMäISTääN NIIN KUIN ITSEääN PAAVALI KERTOO RAKKAUDESTA ENSIMMäISESSä KORINTTILAISKIRJEESSä KIRJEEN TUNNETTUJA KOHTIA OVAT MUUN MUASSA VAIKKA MINä PUHUISIN IHMISTEN ENKELIEN KIELILLä MUTTA MINULTA PUUTTUISI RAKKAUS OLISIN VAIN KUMISEVA VASKI HELISEVä SYMBAALI RAKKAUS KäRSIVäLLINEN RAKKAUS LEMPEä RAKKAUS KADEHDI KERSKU PöYHKEILE KäYTTäYDY SOPIMATTOMASTI ETSI OMAA ETUAAN KATKEROIDU MUISTELE KäRSIMääNSä PAHAA ILOITSE VääRYYDESTä VAAN ILOITSEE TOTUUDEN VOITTAESSA KAIKEN KESTää KAIKESSA USKOO KAIKESSA TOIVOO KAIKEN KäRSII NIIN PYSYVäT NäMä KOLME USKO TOIVO RAKKAUS MUTTA SUURIN NIISTä RAKKAUS ISLAM MUOKKAA MUOKKAA WIKITEKSTIä ISLAMILAISEN MAAILMANKATSOMUKSEN MUKAAN RAKKAUS KAIKKIA USKOSSA OLEVIA YHDISTäVä SIDE VAIKKA JUMALAA SUORAAN KUTSUTA RAKKAUDEKSI YKSI JUMALAN NIMISTä AL-WADUD RAKASTAVA KAIKEN RAKKAUDEN LäHDE JUMALA RAKASTAA JOKAISTA JUMALAAN USKOVAA JOSKIN KUINKA USKOVA ITSE MIELLYTTää JUMALAA TOTEUTTAMALLA HäNEN TAHTOAAN RIIPPUU YKSILöSTä ITSESTääN JUMALAN RAKKAUS IHMISKUNTAA KOHTAAN TODENTUU YKSILöLLE RUKOILUN MIETISKELYN OMISTAUTUMISTA OSOITTAVIEN TEKOJEN KAUTTA ISHQ JUMALAISEN RAKKAUDEN KäSITE MUOKKAA MUOKKAA WIKITEKSTIä ISLAMIN SUUNTAUKSESSA SUFILAISUUDESSA RAKKAUTTA PIDETä VAIN JUMALALLE KUULUVANA JUMALALLISENA PIIRTEENä VAAN JUMALAN OLEMUKSEN YDIN ISHQ RAKKAUS KOSKEE KAIKKEA OLEMASSA OLEVAA SIELU SIJAITSEE RUUMISSA SYDäMESSä ASUU SIELUN LISäKSI RAKKAUS RAKKAUS ASETTUU KAIKEN MAALLISEN JäRJELLISEN YLäPUOLELLE TODELLINEN RAKKAUS KAHDEN IHMISEN VäLILLä TäYDELLISEEN YHTEYTEEN RAKASTUNEET TOTEUTTAVAT JUMALAN OLEMASSA OLOA MAAN PääLLä SEKä RAKASTAVAN ETTä RAKASTETUN TAUSTALLA RAKKAUS RAKASTAVA ONKIN HENKI JOKA EROTETTU RAKASTETUSTAAN JOKA KAIPAA TAKAISIN RAKASTETTU PUOLESTAAN JAMAL TäYDELLISEN KAUNEUDEN ILMENTYMä JOKA NäYTTäYTYY RAKASTAVALLE KUTSUEN TäMäN TAKAISIN ALKULäHTEESEENSä RAKKAUS VALTAA RAKASTUNEEN SYDäMEN TUHOTEN SIELTä KAIKEN YLIMääRäISEN VAIN RAKASTETTU TäRKEä RAKASTAVA LUOPUNUT OMASTA ITSESTääN SAAVUTTAA FANAN TILAN JOSSA SUHTEELLISEN OLEMASSAOLON TILALLE ASTUNUT TäYDELLINEN OLEMASSAOLO TäMäN TAPAHTUMAN MAHDOLLISTAMANA SEURAA TAWHID TäYDELLINEN YHTEYS TäYDELLINEN RAKKAUS KATSO MYöS MUOKKAA MUOKKAA WIKITEKSTIä HALAAMINEN IHMISSUHDE PAIJAAMINEN PARISUHDE SEKSI SEURUSTELU SUUDELMA YSTäVYYS LäHTEET MUOKKAA MUOKKAA WIKITEKSTIä SIIRRY YLöS KIELITOIMISTON SANAKIRJA KOTIMAISTEN KIELTEN TUTKIMUSKESKUKSEN JULKAISUJA INTERNET-VERSIO KIELITOIMISTON SANAKIRJA HELSINKI KOTIMAISTEN KIELTEN TUTKIMUSKESKUS KIELIKONE ISBN SIIRRY YLöS CICOVACKI EROS PHILIA AGAPE AMOR TEOKSESSA MAGNELL THOMAS EXPLORATIONS VALUE AMSTERDAM RODOPI ISBN ENGLANNIKSI SIIRRY YLöS STODDART MICHAEL KIELLETTY HIMOTTAVA HAJU TIEDE SIIRRY YLöS MATT SIIRRY YLöS SIIRRY YLöS SIIRRY YLöS SIIRRY YLöS AL-WADûD SUURAT BEAUTIFUL NAMES ALLAH LONGMONT COLORADO WAHIDUDDIN RICHARD SHELQUIST VIITATTU ENGLANNIKSI SIIRRY YLöS GREENBERG YUDIT KORNBERG TOIM ENCYCLOPEDIA LOVE WORLD RELIGIONS VOLUME SANTA BARBARA CALIFORNIA ABC-CLIO ISBN ENGLANNIKSI SIIRRY YLöS CORNELL VINCENT VOICES ISLAM VOICES SPIRIT WESTPORT CONNECTICUT GREENWOOD PUBLISHING GROUP ISBN ENGLANNIKSI SIIRRY YLöS GREENBERG YUDIT KORNBERG TOIM ENCYCLOPEDIA LOVE WORLD RELIGIONS VOLUME SANTA BARBARA CALIFORNIA ABC-CLIO ISBN ENGLANNIKSI KIRJALLISUUTTA MUOKKAA MUOKKAA WIKITEKSTIä ALBERONI FRANCESCO RAKASTUMINEN INNAMORAMENTO AMORE SUOMENTANEET ULLA RANTA LIISA RYöMä HELSINGISSä OTAVA ISBN HJELM TITUS PASSIO RAKKAUDEN SEKSIN SEURUSTELUN FILOSOFIAA NUORILLE HELSINKI TAMMI ISBN KAST RAKKAUDEN SELITYS LIEBE SICH LEIDENSCHAFT ERKLäRT SUOMENTANUT SARI-ANNE AHVONEN HELSINGISSä AJATUS ISBN LANCELIN AUDE LEMONNIER MARIE FILOSOFIT RAKKAUS PHILOSOPHES L'AMOUR AIMER SOCRATE SIMONE BEAUVOIR SUOMENTANUT TIINA ARPPE HELSINGISSä OTAVA ISBN TAMMISALO OSMO RAKKAUDEN EVOLUUTIO IHMISEN PARINVALINNAN BIOLOGIAA HELSINKI TERRA COGNITA ISBN MääTTä KARINA UUSIAUTTI SATU MANY FACES LOVE SENSE PUBLISHERS ISBN ENGLANNIKSI AIHEESTA MUUALLA MUOKKAA MUOKKAA WIKITEKSTIä OUDOT TUNTEET RAKASTUMINEN OPPIMINEN PHILOSOPHY LOVE INTERNET ENCYCLOPEDIA PHILOSOPHY ENGLANNIKSI ALEX GUNZ ANATOMY LOVE IN-MIND ENGLANNIKSI VENLA PöYLIö KUKA KEKSI RAKKAUDEN TURUN YLIOPPILASLEHTI TäMä PSYKOLOGIAAN LáSKA SYMBOL ROZCESTIA INýCH VýZNAMOCH VýRAZU LáSKA POZRI LáSKA ROZLIšOVACIA STRáNKA SRDCE SYMBOL LáSKY SLOVO LáSKA MôžE VIAC VýZNAMOV INTENZíVNY EMOCIáLNY POCIT NáKLONNOSTI NEJAKEJ OSOBE NAPR MATERSKá LáSKA BOžIA LáSKA LáSKA VäZBA ITEJ OSOBE ZALOžENá SILNEJ TELESNEJ DUCHOVNEJ ALEBO DUšEVNEJ AžLIVOSTI SPRAVIDLA SPOJENá žELANíM DANOU OSOBOU SPOLU NAPR LáSKA PARTNEROVI PLATONICKá LáSKA LáSKA PRVý SEXUáLNY STYK HOVOROVO PREDMET LáSKY NAPR MOJA LáSKA SILNý CITOVý VECI MYšLIENKE NAPR LáSKA PENIAZOM LáSKA ZDRAVIU POHODE LáSKA PRíRODE LáSKA JEDLU LáSKA šPORTU LáSKA VLASTI PSYCHOLOGICKéHO ADISKA RADí MEDZI PRIMáRNE UDSKé POTREBY SVOJ PSYCHOLOGICKý VýZNAM LáSKA JEDNýM NAJDôLEžITEJšíCH NáMETOV UMENí FILMOV OPISUJE PRíBEH LáSKY šINA POPULáRNEJ HUDBY LáSKE FORIEM LáSKY TYPOV MILUJúCICH LáSKA EXISTUJE VšETKýCH KULTúRACH LáSKY EXISTUJúCI DANEJ KULTúRE NAZNA INDIVIDUáLNE CHáPANIE LáSKA RôZNI UDIA HODNOTIA RôZNE TYPY LáSKY ODLIšNE LáSKA ABSTRAKTNá EXISTUJE OKOLO MNOHO OTáZOK SVäTéHO VALENTíNA ANGLOSASKýCH ZEMIACH OSLAVOVANý SVIATOK LáSKY JEDNO ZOBRAZENí LáSKY AMOR SYMBOL PARTNERSKEJ LáSKY PARTNERSKá LáSKA ZVIERACIA LáSKA OBSAH SKRY LáSKA MEDZI INTERPERSONáLNA NáZORY LáSKU BENEDIKT FROMM HESIODOS MARX SYNKRITICIZMUS WILLWOLL LáSKA ZOZNAM LITERATúRY POZRI LáSKA MEDZI LáSKA ENTITY KONTEXTU TYPY LáSKY FíLIE POZRI PROJEKTY EXTERNé ODKAZY LáSKA MEDZI INTERPERSONáLNA UPRAVI UPRAVI ZDROJ INTERPERSONáLNA LáSKA LáSKA MEDZI ZNAMENá VIAC NIEKTO NIEKOMU HOCI POCITY OBVYKLE VZáJOMNé MôžE VZNIKNú NEOPäTOVANá LáSKA INTERPERSONáLNA LáSKA EXISTUJE OBVYKLE INTERPERSONáLNYCH AHOCH NAPR MEDZI PáRMI LENMI RODINY PRIATE UDIA ASTO VYJADRUJú LáSKU INýM OSOBáM MIMO TýCHTO AHOV NAPR RôZNYMI DARMI ALEBO DOBROVO NíCTVOM NIEKTORé PRVKY ASTO PRíTOMNé INTERPERSONáLNEJ LáSKE NáKLONNOS UZNANIE DRUHéHO PREPOJENOS USPOKOJOVANIE ZáKLADNýCH EMOCIONáLNYCH POTRIEB VZáJOMNOS LáSKA VZáJOMNá ZáVäZOK SNAHA UDRžA LáSKU EMOCIONáLNA INTIMITA ZDIE ANIE EMóCIí POCITOV PRíBUZENSTVO RODINNé VäZBY VášE SEXUáLNA TúžBA FYZICKá INTIMITA ZDIE ANIE OSOBNéHO PRIESTORU STAROSTLIVOS SNAHA POMôC SEXUáLNA ENERGIA MôžE NAJDôLEžITEJšíM PRVKOM UJúCIM FORMU ZATIA SEXUáLNA AžLIVOS ASTO PODNECUJE NOVú VäZBU SEXUáLNY POVAžOVANý NEžIADúCI ALEBO NEVHODNý ITýCH VäZBáCH LáSKY MNOHO ETICKýCH SYSTéMOV ODSUDZUJE SEXUáLNE MEDZI LENMI RODINY ARTIKKELI TYNKä VOIT AUTTAA WIKIPEDIAA LAAJENTAMALLA ARTIKKELIA LUOKAT TUNTEETHYVEET SLOVAKI PORESTIN OCCIALà ITSKýCHONSK VOKSI PORTUGUE VIERöIMIA SOTTAMPLE SLOVANU KEROX HISIMIA NäYTEESSAND IERNEWEK úDATACHO LIETUGUE VOKANOU SLOVAKISH GàIDANILAA TIENä' OMAN TRVAKIPETI ABECHONS ZASTUKSTUISH NáROON LäNTèIS LIUDU 'SUUN HRVAKKI SLOVENUTON HISENš SEDA INDATTU UKRATINEN OLLYSTYVILI PIEDOV MUURU ZAHIN NäISKéHO LATINEJ ESIMBURI MEDENé TüRKIN íTAMOC SLOVESSä ROZG SáMEä 'HES KNASTIA NENIEN VASIINEJ MUUVIGáCH GALT KIRO DIFTORIA ABECEDIFORí AKAANKU LUETTUNA DEVAKENORSKEI' ENGLI UNIE SLOVEHO NáROJVODIáLNOA VALAMBURTEMISLU DOBNýCHáDZI VASTEESTRáNO 'MIELENSUTO MULGARPANTA KOVAKILI SUUTOR RAIN FROM WIKIPEDIA FREE ENCYCLOPEDIA OTHER USES RAIN DISAMBIGUATION RAINY DISAMBIGUATION BLACK STORM CLOUDS UNDER WHICH GREY SHEET RAIN FALLING GRASSLANDS RAIN SHAFT BASE THUNDERSTORM TORRENTIAL RAIN PART NATURE SERIES WEATHER CALENDAR SEASONS WINTER SPRING SUMMER AUTUMN TROPICAL SEASONS SEASON SEASON STORMS BLIZZARD CLOUD DOWNBURST DUST STORM EXTRATROPICAL CYCLONE FIRESTORM STORM LIGHTNING SUPERCELL THUNDERSTORM THUNDERSNOW TORNADO TROPICAL CYCLONE HURRICANE WATERSPOUT WINTER STORM PRECIPITATION DRIZZLE FREEZING DRIZZLE GRAUPEL HAIL PELLETS DIAMOND DUST RAIN FREEZING RAIN SNOW RAIN SNOW MIXED SNOW GRAINS SNOW ROLLER SLUSH TOPICS POLLUTION CLIMATE CLOUD COLD WAVE HEAT WAVE METEOROLOGY SEVERE WEATHER WEATHER FORECASTING PORTAL ICON WEATHER PORTAL RAIN MENU TYPICAL SOUND RAIN WITH THUNDER PROBLEMS PLAYING THIS FILE MEDIA HELP RAIN LIQUID WATER FORM DROPLETS THAT HAVE CONDENSED FROM ATMOSPHERIC WATER VAPOR THEN PRECIPITATED—THAT BECOME HEAVY ENOUGH FALL UNDER GRAVITY RAIN MAJOR COMPONENT WATER CYCLE RESPONSIBLE DEPOSITING MOST FRESH WATER EARTH PROVIDES SUITABLE CONDITIONS MANY TYPES ECOSYSTEMS WELL WATER HYDROELECTRIC POWER PLANTS CROP IRRIGATION MAJOR CAUSE RAIN PRODUCTION MOISTURE MOVING ALONG THREE-DIMENSIONAL ZONES TEMPERATURE MOISTURE CONTRASTS KNOWN WEATHER FRONTS ENOUGH MOISTURE UPWARD MOTION PRESENT PRECIPITATION FALLS FROM CONVECTIVE CLOUDS THOSE WITH STRONG UPWARD VERTICAL MOTION SUCH CUMULONIMBUS THUNDER CLOUDS WHICH ORGANIZE INTO NARROW RAINBANDS MOUNTAINOUS AREAS HEAVY PRECIPITATION POSSIBLE WHERE UPSLOPE FLOW MAXIMIZED WITHIN WINDWARD SIDES TERRAIN ELEVATION WHICH FORCES MOIST CONDENSE FALL RAINFALL ALONG SIDES MOUNTAINS LEEWARD SIDE MOUNTAINS DESERT CLIMATES EXIST CAUSED DOWNSLOPE FLOW WHICH CAUSES HEATING DRYING MASS MOVEMENT MONSOON TROUGH INTERTROPICAL CONVERGENCE ZONE BRINGS RAINY SEASONS SAVANNAH CLIMES URBAN HEAT ISLAND EFFECT LEADS INCREASED RAINFALL BOTH AMOUNTS INTENSITY DOWNWIND CITIES GLOBAL WARMING ALSO CAUSING CHANGES PRECIPITATION PATTERN GLOBALLY INCLUDING WETTER CONDITIONS ACROSS EASTERN NORTH AMERICA DRIER CONDITIONS TROPICS CITATION NEEDED ANTARCTICA DRIEST CONTINENT GLOBALLY AVERAGED ANNUAL PRECIPITATION OVER LAND OVER WHOLE EARTH MUCH HIGHER CLIMATE CLASSIFICATION SYSTEMS SUCH KöPPEN CLIMATE CLASSIFICATION SYSTEM AVERAGE ANNUAL RAINFALL HELP DIFFERENTIATE BETWEEN DIFFERING CLIMATE REGIMES RAINFALL MEASURED USING RAIN GAUGES RAINFALL AMOUNTS ESTIMATED WEATHER RADAR RAIN ALSO KNOWN SUSPECTED OTHER PLANETS WHERE COMPOSED METHANE NEON SULFURIC ACID EVEN IRON RATHER THAN WATER CONTENTS HIDE FORMATION WATER-SATURATED COALESCENCE FRAGMENTATION DROPLET SIZE DISTRIBUTION RAINDROP IMPACTS VIRGA CAUSES FRONTAL ACTIVITY CONVECTION OROGRAPHIC EFFECTS WITHIN TROPICS HUMAN INFLUENCE CHARACTERISTICS PATTERNS ACIDITY KöPPEN CLIMATE CLASSIFICATION MEASUREMENT GAUGES REMOTE SENSING INTENSITY RETURN PERIOD FORECASTING IMPACT EFFECT AGRICULTURE CULTURE GLOBAL CLIMATOLOGY DESERTS POLAR DESERT RAINFORESTS MONSOONS IMPACT WESTERLIES WETTEST KNOWN LOCATIONS OUTSIDE EARTH ALSO NOTES REFERENCES EXTERNAL LINKS FORMATION WATER-SATURATED CONTAINS WATER VAPOR AMOUNT WATER GIVEN MASS KNOWN MIXING RATIO MEASURED GRAMS WATER KILOGRAM AMOUNT MOISTURE ALSO COMMONLY REPORTED RELATIVE HUMIDITY WHICH PERCENTAGE TOTAL WATER VAPOR HOLD PARTICULAR TEMPERATURE MUCH WATER VAPOR PARCEL CONTAIN BEFORE BECOMES SATURATED RELATIVE HUMIDITY FORMS INTO CLOUD GROUP VISIBLE TINY WATER PARTICLES SUSPENDED ABOVE EARTH'S SURFACE DEPENDS TEMPERATURE WARMER CONTAIN MORE WATER VAPOR THAN COOLER BEFORE BECOMING SATURATED THEREFORE SATURATE PARCEL COOL POINT TEMPERATURE WHICH PARCEL MUST COOLED ORDER BECOME SATURATED THERE FOUR MAIN MECHANISMS COOLING POINT ADIABATIC COOLING CONDUCTIVE COOLING RADIATIONAL COOLING EVAPORATIVE COOLING ADIABATIC COOLING OCCURS WHEN RISES EXPANDS RISE CONVECTION LARGE-SCALE ATMOSPHERIC MOTIONS PHYSICAL BARRIER SUCH MOUNTAIN OROGRAPHIC LIFT CONDUCTIVE COOLING OCCURS WHEN COMES INTO CONTACT WITH COLDER SURFACE USUALLY BEING BLOWN FROM SURFACE ANOTHER EXAMPLE FROM LIQUID WATER SURFACE COLDER LAND RADIATIONAL COOLING OCCURS EMISSION INFRARED RADIATION EITHER SURFACE UNDERNEATH EVAPORATIVE COOLING OCCURS WHEN MOISTURE ADDED THROUGH EVAPORATION WHICH FORCES TEMPERATURE COOL WET-BULB TEMPERATURE UNTIL REACHES SATURATION MAIN WAYS WATER VAPOR ADDED WIND CONVERGENCE INTO AREAS UPWARD MOTION PRECIPITATION VIRGA FALLING FROM ABOVE DAYTIME HEATING EVAPORATING WATER FROM SURFACE OCEANS WATER BODIES LAND TRANSPIRATION FROM PLANTS COOL MOVING OVER WARMER WATER LIFTING OVER MOUNTAINS WATER VAPOR NORMALLY BEGINS CONDENSE CONDENSATION NUCLEI SUCH DUST SALT ORDER FORM CLOUDS ELEVATED PORTIONS WEATHER FRONTS WHICH THREE-DIMENSIONAL NATURE FORCE BROAD AREAS UPWARD MOTION WITHIN EARTH'S ATMOSPHERE WHICH FORM CLOUDS DECKS SUCH ALTOSTRATUS CIRROSTRATUS STRATUS STABLE CLOUD DECK WHICH TENDS FORM WHEN COOL STABLE MASS TRAPPED UNDERNEATH WARM MASS ALSO FORM LIFTING ADVECTION DURING BREEZY CONDITIONS COALESCENCE FRAGMENTATION DIAGRAM SHOWING THAT VERY SMALL RAIN DROPS ALMOST SPHERICAL SHAPE DROPS BECOME LARGER THEY BECOME FLATTENED BOTTOM LIKE HAMBURGER VERY LARGE RAIN DROPS SPLIT INTO SMALLER ONES RESISTANCE WHICH MAKES THEM INCREASINGLY UNSTABLE SHAPE RAIN DROPS DEPENDING UPON THEIR SIZE COALESCENCE OCCURS WHEN WATER DROPLETS FUSE CREATE LARGER WATER DROPLETS RESISTANCE TYPICALLY CAUSES WATER DROPLETS CLOUD REMAIN STATIONARY WHEN TURBULENCE OCCURS WATER DROPLETS COLLIDE PRODUCING LARGER DROPLETS THESE LARGER WATER DROPLETS DESCEND COALESCENCE CONTINUES THAT DROPS BECOME HEAVY ENOUGH OVERCOME RESISTANCE FALL RAIN COALESCENCE GENERALLY HAPPENS MOST OFTEN CLOUDS ABOVE FREEZING ALSO KNOWN WARM RAIN PROCESS CLOUDS BELOW FREEZING WHEN CRYSTALS GAIN ENOUGH MASS THEY BEGIN FALL THIS GENERALLY REQUIRES MORE MASS THAN COALESCENCE WHEN OCCURRING BETWEEN CRYSTAL NEIGHBORING WATER DROPLETS THIS PROCESS TEMPERATURE DEPENDENT SUPERCOOLED WATER DROPLETS ONLY EXIST CLOUD THAT BELOW FREEZING ADDITION BECAUSE GREAT TEMPERATURE DIFFERENCE BETWEEN CLOUD GROUND LEVEL THESE CRYSTALS MELT THEY FALL BECOME RAIN RAINDROPS HAVE SIZES RANGING FROM MEAN DIAMETER ABOVE WHICH THEY TEND BREAK SMALLER DROPS CALLED CLOUD DROPLETS THEIR SHAPE SPHERICAL RAINDROP INCREASES SIZE SHAPE BECOMES MORE OBLATE WITH LARGEST CROSS-SECTION FACING ONCOMING AIRFLOW LARGE RAIN DROPS BECOME INCREASINGLY FLATTENED BOTTOM LIKE HAMBURGER BUNS VERY LARGE ONES SHAPED LIKE PARACHUTES CONTRARY POPULAR BELIEF THEIR SHAPE DOES RESEMBLE TEARDROP BIGGEST RAINDROPS EARTH WERE RECORDED OVER BRAZIL MARSHALL ISLANDS SOME THEM WERE LARGE LARGE SIZE EXPLAINED CONDENSATION LARGE SMOKE PARTICLES COLLISIONS BETWEEN DROPS SMALL REGIONS WITH PARTICULARLY HIGH CONTENT LIQUID WATER RAIN DROPS ASSOCIATED WITH MELTING HAIL TEND LARGER THAN OTHER RAIN DROPS RAINDROP RAINDROP LEAF INTENSITY DURATION RAINFALL USUALLY INVERSELY RELATED HIGH INTENSITY STORMS LIKELY SHORT DURATION INTENSITY STORMS HAVE LONG DURATION DROPLET SIZE DISTRIBUTION FINAL DROPLET SIZE DISTRIBUTION EXPONENTIAL DISTRIBUTION NUMBER DROPLETS WITH DIAMETER BETWEEN DISPLAYSTYLE DISPLAYSTYLE UNIT VOLUME SPACE DISPLAYSTYLE LANGLE RANGLE LANGLE RANGLE THIS COMMONLY REFERRED MARSHALL–PALMER AFTER RESEARCHERS FIRST CHARACTERIZED PARAMETERS SOMEWHAT TEMPERATURE-DEPENDENT SLOPE ALSO SCALES WITH RATE RAINFALL DISPLAYSTYLE LANGLE RANGLE LANGLE RANGLE CENTIMETERS MILLIMETRES HOUR DEVIATIONS OCCUR SMALL DROPLETS DURING DIFFERENT RAINFALL CONDITIONS DISTRIBUTION TENDS AVERAGED RAINFALL WHILE INSTANTANEOUS SIZE SPECTRA OFTEN DEVIATE HAVE BEEN MODELED GAMMA DISTRIBUTIONS DISTRIBUTION UPPER LIMIT DROPLET FRAGMENTATION RAINDROP IMPACTS RAINDROPS IMPACT THEIR TERMINAL VELOCITY WHICH GREATER LARGER DROPS THEIR LARGER MASS DRAG RATIO LEVEL WITHOUT WIND DRIZZLE IMPACTS WHILE LARGE DROPS IMPACT AROUND RAIN FALLING LOOSELY PACKED MATERIAL SUCH NEWLY FALLEN PRODUCE DIMPLES THAT FOSSILIZED DENSITY DEPENDENCE MAXIMUM RAINDROP DIAMETER TOGETHER WITH FOSSIL RAINDROP IMPRINTS BEEN USED CONSTRAIN DENSITY BILLION YEARS SOUND RAINDROPS HITTING WATER CAUSED BUBBLES OSCILLATING UNDERWATER METAR CODE RAIN WHILE CODING RAIN SHOWERS SHRA VIRGA CERTAIN CONDITIONS PRECIPITATION FALL FROM CLOUD THEN EVAPORATES SUBLIMES BEFORE REACHING GROUND THIS TERMED VIRGA MORE OFTEN SEEN CLIMATES CAUSES FRONTAL ACTIVITY MAIN ARTICLE WEATHER FRONTS STRATIFORM BROAD SHIELD PRECIPITATION WITH RELATIVELY SIMILAR INTENSITY DYNAMIC PRECIPITATION CONVECTIVE PRECIPITATION WHICH SHOWERY NATURE WITH LARGE CHANGES INTENSITY OVER SHORT DISTANCES OCCUR CONSEQUENCE SLOW ASCENT SYNOPTIC SYSTEMS ORDER SUCH VICINITY COLD FRONTS NEAR POLEWARD SURFACE WARM FRONTS SIMILAR ASCENT SEEN AROUND TROPICAL CYCLONES OUTSIDE EYEWALL COMMA-HEAD PRECIPITATION PATTERNS AROUND MID-LATITUDE CYCLONES WIDE VARIETY WEATHER FOUND ALONG OCCLUDED FRONT WITH THUNDERSTORMS POSSIBLE USUALLY THEIR PASSAGE ASSOCIATED WITH DRYING MASS OCCLUDED FRONTS USUALLY FORM AROUND MATURE LOW-PRESSURE AREAS WHAT SEPARATES RAINFALL FROM OTHER PRECIPITATION TYPES SUCH PELLETS SNOW PRESENCE THICK LAYER ALOFT WHICH ABOVE MELTING POINT WATER WHICH MELTS FROZEN PRECIPITATION WELL BEFORE REACHES GROUND THERE SHALLOW NEAR SURFACE LAYER THAT BELOW FREEZING FREEZING RAIN RAIN WHICH FREEZES CONTACT WITH SURFACES SUBFREEZING ENVIRONMENTS WILL RESULT HAIL BECOMES INCREASINGLY INFREQUENT OCCURRENCE WHEN FREEZING LEVEL WITHIN ATMOSPHERE EXCEEDS ABOVE GROUND LEVEL CONVECTION DIAGRAM SHOWING THAT MOIST BECOMES HEATED MORE THAN SURROUNDINGS MOVES UPWARD RESULTING BRIEF RAIN SHOWERS CONVECTIVE PRECIPITATION DIAGRAM SHOWING MOIST OVER OCEAN RISES FLOWS OVER LAND CAUSING COOLING RAIN HITS MOUNTAIN RIDGES OROGRAPHIC PRECIPITATION CONVECTIVE RAIN SHOWERY PRECIPITATION OCCURS FROM CONVECTIVE CLOUDS CUMULONIMBUS CUMULUS CONGESTUS FALLS SHOWERS WITH RAPIDLY CHANGING INTENSITY CONVECTIVE PRECIPITATION FALLS OVER CERTAIN AREA RELATIVELY SHORT TIME CONVECTIVE CLOUDS HAVE LIMITED HORIZONTAL EXTENT MOST PRECIPITATION TROPICS APPEARS CONVECTIVE HOWEVER BEEN SUGGESTED THAT STRATIFORM PRECIPITATION ALSO OCCURS GRAUPEL HAIL INDICATE CONVECTION MID-LATITUDES CONVECTIVE PRECIPITATION INTERMITTENT OFTEN ASSOCIATED WITH BAROCLINIC BOUNDARIES SUCH COLD FRONTS SQUALL LINES WARM FRONTS OROGRAPHIC EFFECTS MAIN ARTICLES OROGRAPHIC LIFT PRECIPITATION TYPES METEOROLOGY UNITED STATES RAINFALL CLIMATOLOGY OROGRAPHIC PRECIPITATION OCCURS WINDWARD SIDE MOUNTAINS CAUSED RISING MOTION LARGE-SCALE FLOW MOIST ACROSS MOUNTAIN RIDGE RESULTING ADIABATIC COOLING CONDENSATION MOUNTAINOUS PARTS WORLD SUBJECTED RELATIVELY CONSISTENT WINDS EXAMPLE TRADE WINDS MORE MOIST CLIMATE USUALLY PREVAILS WINDWARD SIDE MOUNTAIN THAN LEEWARD DOWNWIND SIDE MOISTURE REMOVED OROGRAPHIC LIFT LEAVING DRIER KATABATIC WIND DESCENDING GENERALLY WARMING LEEWARD SIDE WHERE RAIN SHADOW OBSERVED HAWAII MOUNT ISLAND KAUAI NOTABLE EXTREME RAINFALL SECOND HIGHEST AVERAGE ANNUAL RAINFALL EARTH WITH SYSTEMS KNOWN KONA STORMS AFFECT STATE WITH HEAVY RAINS BETWEEN OCTOBER APRIL LOCAL CLIMATES VARY CONSIDERABLY EACH ISLAND THEIR TOPOGRAPHY DIVISIBLE INTO WINDWARD OLAU LEEWARD KONA REGIONS BASED UPON LOCATION RELATIVE HIGHER MOUNTAINS WINDWARD SIDES FACE EAST NORTHEAST TRADE WINDS RECEIVE MUCH MORE RAINFALL LEEWARD SIDES DRIER SUNNIER WITH LESS RAIN LESS CLOUD COVER SOUTH AMERICA ANDES MOUNTAIN RANGE BLOCKS PACIFIC MOISTURE THAT ARRIVES THAT CONTINENT RESULTING DESERTLIKE CLIMATE JUST DOWNWIND ACROSS WESTERN ARGENTINA SIERRA NEVADA RANGE CREATES SAME EFFECT NORTH AMERICA FORMING GREAT BASIN MOJAVE DESERTS WITHIN TROPICS CHART SHOWING AUSTRALIAN CITY WITH MUCH RAIN WINTER MONTHS LESS THAN SUMMER RAINFALL DISTRIBUTION MONTH CAIRNS SHOWING EXTENT SEASON THAT LOCATION ALSO MONSOON TROPICAL CYCLONE MAIN ARTICLE SEASON RAINY SEASON TIME YEAR COVERING MORE MONTHS WHEN MOST AVERAGE ANNUAL RAINFALL REGION FALLS TERM GREEN SEASON ALSO SOMETIMES USED EUPHEMISM TOURIST AUTHORITIES AREAS WITH SEASONS DISPERSED ACROSS PORTIONS TROPICS SUBTROPICS SAVANNA CLIMATES AREAS WITH MONSOON REGIMES HAVE SUMMERS WINTERS TROPICAL RAINFORESTS TECHNICALLY HAVE SEASONS SINCE THEIR RAINFALL EQUALLY DISTRIBUTED THROUGH YEAR SOME AREAS WITH PRONOUNCED RAINY SEASONS WILL BREAK RAINFALL MID-SEASON WHEN INTERTROPICAL CONVERGENCE ZONE MONSOON TROUGH MOVE POLEWARD THEIR LOCATION DURING MIDDLE WARM SEASON WHEN SEASON OCCURS DURING WARM SEASON SUMMER RAIN FALLS MAINLY DURING LATE AFTERNOON EARLY EVENING HOURS SEASON TIME WHEN QUALITY IMPROVES FRESHWATER QUALITY IMPROVES VEGETATION GROWS SIGNIFICANTLY TROPICAL CYCLONES SOURCE VERY HEAVY RAINFALL CONSIST LARGE MASSES SEVERAL HUNDRED MILES ACROSS WITH PRESSURE CENTRE WITH WINDS BLOWING INWARD TOWARDS CENTRE EITHER CLOCKWISE DIRECTION SOUTHERN HEMISPHERE COUNTER CLOCKWISE NORTHERN HEMISPHERE ALTHOUGH CYCLONES TAKE ENORMOUS TOLL LIVES PERSONAL PROPERTY THEY IMPORTANT FACTORS PRECIPITATION REGIMES PLACES THEY IMPACT THEY BRING MUCH-NEEDED PRECIPITATION OTHERWISE REGIONS AREAS THEIR PATH RECEIVE YEAR'S WORTH RAINFALL FROM TROPICAL CYCLONE PASSAGE HUMAN INFLUENCE IMAGE ATLANTA GEORGIA SHOWING TEMPERATURE DISTRIBUTION WITH BLUE SHOWING COOL TEMPERATURES WARM AREAS APPEAR WHITE WORLD TEMPERATURE DISTRIBUTION SHOWS NORTHERN HEMISPHERE WARMER THAN SOUTHERN HEMISPHERE DURING PERIODS COMPARED MEAN SURFACE TEMPERATURE ANOMALIES DURING PERIOD WITH RESPECT AVERAGE TEMPERATURES FROM ALSO GLOBAL WARMING URBAN HEAT ISLAND FINE PARTICULATE MATTER PRODUCED EXHAUST OTHER HUMAN SOURCES POLLUTION FORMS CLOUD CONDENSATION NUCLEI LEADS PRODUCTION CLOUDS INCREASES LIKELIHOOD RAIN COMMUTERS COMMERCIAL TRAFFIC CAUSE POLLUTION BUILD OVER COURSE WEEK LIKELIHOOD RAIN INCREASES PEAKS SATURDAY AFTER FIVE DAYS WEEKDAY POLLUTION BEEN BUILT HEAVILY POPULATED AREAS THAT NEAR COAST SUCH UNITED STATES' EASTERN SEABOARD EFFECT DRAMATIC THERE HIGHER CHANCE RAIN SATURDAYS THAN MONDAYS URBAN HEAT ISLAND EFFECT WARMS CITIES ABOVE SURROUNDING SUBURBS RURAL AREAS THIS EXTRA HEAT LEADS GREATER UPWARD MOTION WHICH INDUCE ADDITIONAL SHOWER THUNDERSTORM ACTIVITY RAINFALL RATES DOWNWIND CITIES INCREASED BETWEEN PARTLY RESULT THIS WARMING MONTHLY RAINFALL ABOUT GREATER BETWEEN DOWNWIND CITIES COMPARED WITH UPWIND SOME CITIES INDUCE TOTAL PRECIPITATION INCREASE INCREASING TEMPERATURES TEND INCREASE EVAPORATION WHICH LEAD MORE PRECIPITATION PRECIPITATION GENERALLY INCREASED OVER LAND NORTH FROM THROUGH DECLINED OVER TROPICS SINCE GLOBALLY THERE BEEN STATISTICALLY SIGNIFICANT OVERALL TREND PRECIPITATION OVER PAST CENTURY ALTHOUGH TRENDS HAVE VARIED WIDELY REGION OVER TIME EASTERN PORTIONS NORTH SOUTH AMERICA NORTHERN EUROPE NORTHERN CENTRAL ASIA HAVE BECOME WETTER SAHEL MEDITERRANEAN SOUTHERN AFRICA PARTS SOUTHERN ASIA HAVE BECOME DRIER THERE BEEN INCREASE NUMBER HEAVY PRECIPITATION EVENTS OVER MANY AREAS DURING PAST CENTURY WELL INCREASE SINCE PREVALENCE DROUGHTS—ESPECIALLY TROPICS SUBTROPICS CHANGES PRECIPITATION EVAPORATION OVER OCEANS SUGGESTED DECREASED SALINITY MID- HIGH-LATITUDE WATERS IMPLYING MORE PRECIPITATION ALONG WITH INCREASED SALINITY LOWER LATITUDES IMPLYING LESS PRECIPITATION MORE EVAPORATION OVER CONTIGUOUS UNITED STATES TOTAL ANNUAL PRECIPITATION INCREASED AVERAGE RATE PERCENT SINCE WITH GREATEST INCREASES WITHIN EAST NORTH CENTRAL CLIMATE REGION PERCENT CENTURY SOUTH PERCENT HAWAII ONLY REGION SHOW DECREASE PERCENT ANALYSIS YEARS UNITED STATES AMERICA RAINFALL RECORDS SHOW LOWER STATES HAVE INCREASE HEAVY DOWNPOURS SINCE LARGEST INCREASES NORTHEAST MIDWEST WHICH PAST DECADE HAVE SEEN PERCENT MORE HEAVY DOWNPOURS COMPARED RHODE ISLAND STATE WITH LARGEST INCREASE MCALLEN TEXAS CITY WITH LARGEST INCREASE HEAVY DOWNPOUR ANALYSIS DAYS WHERE TOTAL PRECIPITATION EXCEEDED PERCENT RAIN SNOW DAYS DURING YEARS MOST SUCCESSFUL ATTEMPTS INFLUENCING WEATHER INVOLVE CLOUD SEEDING WHICH INCLUDE TECHNIQUES USED INCREASE WINTER PRECIPITATION OVER MOUNTAINS SUPPRESS HAIL CHARACTERISTICS PATTERNS BAND THUNDERSTORMS SEEN WEATHER RADAR DISPLAY MAIN ARTICLE RAINBAND RAINBANDS CLOUD PRECIPITATION AREAS WHICH SIGNIFICANTLY ELONGATED RAINBANDS STRATIFORM CONVECTIVE GENERATED DIFFERENCES TEMPERATURE WHEN NOTED WEATHER RADAR IMAGERY THIS PRECIPITATION ELONGATION REFERRED BANDED STRUCTURE RAINBANDS ADVANCE WARM OCCLUDED FRONTS WARM FRONTS ASSOCIATED WITH WEAK UPWARD MOTION TEND WIDE STRATIFORM NATURE RAINBANDS SPAWNED NEAR AHEAD COLD FRONTS SQUALL LINES WHICH ABLE PRODUCE TORNADOES RAINBANDS ASSOCIATED WITH COLD FRONTS WARPED MOUNTAIN BARRIERS PERPENDICULAR FRONT'S ORIENTATION FORMATION LOW-LEVEL BARRIER BANDS THUNDERSTORMS FORM WITH BREEZE LAND BREEZE BOUNDARIES ENOUGH MOISTURE PRESENT BREEZE RAINBANDS BECOME ACTIVE ENOUGH JUST AHEAD COLD FRONT THEY MASK LOCATION COLD FRONT ITSELF ONCE CYCLONE OCCLUDES TROUGH WARM ALOFT TROWAL SHORT WILL CAUSED STRONG SOUTHERLY WINDS EASTERN PERIPHERY ROTATING ALOFT AROUND NORTHEAST ULTIMATELY NORTHWESTERN PERIPHERY ALSO KNOWN WARM CONVEYOR BELT FORCING SURFACE TROUGH CONTINUE INTO COLD SECTOR SIMILAR CURVE OCCLUDED FRONT TROWAL CREATES PORTION OCCLUDED CYCLONE KNOWN COMMA HEAD COMMA-LIKE SHAPE MID-TROPOSPHERIC CLOUDINESS THAT ACCOMPANIES FEATURE ALSO FOCUS LOCALLY HEAVY PRECIPITATION WITH THUNDERSTORMS POSSIBLE ATMOSPHERE ALONG TROWAL UNSTABLE ENOUGH CONVECTION BANDING WITHIN COMMA HEAD PRECIPITATION PATTERN EXTRATROPICAL CYCLONE YIELD SIGNIFICANT AMOUNTS RAIN BEHIND EXTRATROPICAL CYCLONES DURING FALL WINTER RAINBANDS FORM DOWNWIND RELATIVE WARM BODIES WATER SUCH GREAT LAKES DOWNWIND ISLANDS BANDS SHOWERS THUNDERSTORMS DEVELOP LEVEL WIND CONVERGENCE DOWNWIND ISLAND EDGES OFFSHORE CALIFORNIA THIS BEEN NOTED WAKE COLD FRONTS RAINBANDS WITHIN TROPICAL CYCLONES CURVED ORIENTATION TROPICAL CYCLONE RAINBANDS CONTAIN SHOWERS THUNDERSTORMS THAT TOGETHER WITH EYEWALL CONSTITUTE HURRICANE TROPICAL STORM EXTENT RAINBANDS AROUND TROPICAL CYCLONE HELP DETERMINE CYCLONE'S INTENSITY ACIDITY ORIGINS ACID RAIN ALSO ACID RAIN PHRASE ACID RAIN FIRST USED SCOTTISH CHEMIST ROBERT AUGUS SMITH RAIN VARIES ESPECIALLY ORIGIN AMERICA'S EAST COAST RAIN THAT DERIVED FROM ATLANTIC OCEAN TYPICALLY RAIN THAT COMES ACROSS CONTINENTAL FROM WEST LOCAL THUNDERSTORMS HAVE RAIN BECOMES ACIDIC PRIMARILY PRESENCE STRONG ACIDS SULFURIC ACID NITRIC ACID SULFURIC ACID DERIVED FROM NATURAL SOURCES SUCH VOLCANOES WETLANDS SULFATE REDUCING BACTERIA ANTHROPOGENIC SOURCES SUCH COMBUSTION FOSSIL FUELS MINING WHERE PRESENT NITRIC ACID PRODUCED NATURAL SOURCES SUCH LIGHTNING SOIL BACTERIA NATURAL FIRES WHILE ALSO PRODUCED ANTHROPOGENICALLY COMBUSTION FOSSIL FUELS FROM POWER PLANTS PAST YEARS CONCENTRATIONS NITRIC SULFURIC ACID DECREASED PRESENCE RAINWATER WHICH SIGNIFICANT INCREASE AMMONIUM MOST LIKELY AMMONIA FROM LIVESTOCK PRODUCTION WHICH ACTS BUFFER ACID RAIN RAISES KöPPEN CLIMATE CLASSIFICATION UPDATED KöPPEN-GEIGER CLIMATE MAIN ARTICLE KöPPEN CLIMATE CLASSIFICATION KöPPEN CLASSIFICATION DEPENDS AVERAGE MONTHLY VALUES TEMPERATURE PRECIPITATION MOST COMMONLY USED FORM KöPPEN CLASSIFICATION FIVE PRIMARY TYPES LABELED THROUGH SPECIFICALLY PRIMARY TYPES TROPICAL MILD MID-LATITUDE COLD MID-LATITUDE POLAR FIVE PRIMARY CLASSIFICATIONS FURTHER DIVIDED INTO SECONDARY CLASSIFICATIONS SUCH RAIN FOREST MONSOON TROPICAL SAVANNA HUMID SUBTROPICAL HUMID CONTINENTAL OCEANIC CLIMATE MEDITERRANEAN CLIMATE STEPPE SUBARCTIC CLIMATE TUNDRA POLAR DESERT RAIN FORESTS CHARACTERIZED HIGH RAINFALL WITH DEFINITIONS SETTING MINIMUM NORMAL ANNUAL RAINFALL BETWEEN TROPICAL SAVANNA GRASSLAND BIOME LOCATED SEMI-ARID SEMI-HUMID CLIMATE REGIONS SUBTROPICAL TROPICAL LATITUDES WITH RAINFALL BETWEEN YEAR THEY WIDESPREAD AFRICA ALSO FOUND INDIA NORTHERN PARTS SOUTH AMERICA MALAYSIA AUSTRALIA HUMID SUBTROPICAL CLIMATE ZONE WHERE WINTER RAINFALL ASSOCIATED WITH LARGE STORMS THAT WESTERLIES STEER FROM WEST EAST MOST SUMMER RAINFALL OCCURS DURING THUNDERSTORMS FROM OCCASIONAL TROPICAL CYCLONES HUMID SUBTROPICAL CLIMATES EAST SIDE CONTINENTS ROUGHLY BETWEEN LATITUDES DEGREES AWAY FROM EQUATOR OCEANIC MARITIME CLIMATE TYPICALLY FOUND ALONG WEST COASTS MIDDLE LATITUDES WORLD'S CONTINENTS BORDERING COOL OCEANS WELL SOUTHEASTERN AUSTRALIA ACCOMPANIED PLENTIFUL PRECIPITATION YEAR ROUND MEDITERRANEAN CLIMATE REGIME RESEMBLES CLIMATE LANDS MEDITERRANEAN BASIN PARTS WESTERN NORTH AMERICA PARTS WESTERN SOUTH AUSTRALIA SOUTHWESTERN SOUTH AFRICA PARTS CENTRAL CHILE CLIMATE CHARACTERIZED SUMMERS COOL WINTERS STEPPE GRASSLAND SUBARCTIC CLIMATES COLD WITH CONTINUOUS PERMAFROST LITTLE PRECIPITATION MEASUREMENT GAUGES STANDARD RAIN GAUGE ALSO RAIN GAUGE DISDROMETER SNOW GAUGE RAIN MEASURED UNITS LENGTH UNIT TIME TYPICALLY MILLIMETERS HOUR COUNTRIES WHERE IMPERIAL UNITS MORE COMMON INCHES HOUR LENGTH MORE ACCURATELY DEPTH BEING MEASURED DEPTH RAIN WATER THAT WOULD ACCUMULATE FLAT HORIZONTAL IMPERMEABLE SURFACE DURING GIVEN AMOUNT TIME TYPICALLY HOUR MILLIMETER RAINFALL EQUIVALENT LITER WATER SQUARE METER STANDARD MEASURING RAINFALL SNOWFALL STANDARD RAIN GAUGE WHICH FOUND PLASTIC METAL VARIETIES INNER CYLINDER FILLED RAIN WITH OVERFLOW FLOWING INTO OUTER CYLINDER PLASTIC GAUGES HAVE MARKINGS INNER CYLINDER DOWN RESOLUTION WHILE METAL GAUGES REQUIRE STICK DESIGNED WITH APPROPRIATE MARKINGS AFTER INNER CYLINDER FILLED AMOUNT INSIDE DISCARDED THEN FILLED WITH REMAINING RAINFALL OUTER CYLINDER UNTIL FLUID OUTER CYLINDER GONE ADDING OVERALL TOTAL UNTIL OUTER CYLINDER EMPTY OTHER TYPES GAUGES INCLUDE POPULAR WEDGE GAUGE CHEAPEST RAIN GAUGE MOST FRAGILE TIPPING BUCKET RAIN GAUGE WEIGHING RAIN GAUGE THOSE LOOKING MEASURE RAINFALL MOST INEXPENSIVELY THAT CYLINDRICAL WITH STRAIGHT SIDES WILL RAIN GAUGE LEFT OPEN ACCURACY WILL DEPEND WHAT RULER USED MEASURE RAIN WITH ABOVE RAIN GAUGES MADE HOME WITH ENOUGH KNOW-HOW WHEN PRECIPITATION MEASUREMENT MADE VARIOUS NETWORKS EXIST ACROSS UNITED STATES ELSEWHERE WHERE RAINFALL MEASUREMENTS SUBMITTED THROUGH INTERNET SUCH COCORAHS GLOBE NETWORK AVAILABLE AREA WHERE LIVES NEAREST LOCAL WEATHER OFFICE WILL LIKELY INTERESTED MEASUREMENT REMOTE SENSING ALSO WEATHER RADAR TWENTY-FOUR-HOUR RAINFALL ACCUMULATION D'IRèNE RADAR EASTERN CANADA ZONES WITHOUT DATA EAST SOUTHWEST CAUSED BEAM BLOCKING FROM MOUNTAINS SOURCE ENVIRONMENT CANADA MAIN USES WEATHER RADAR ABLE ASSESS AMOUNT PRECIPITATIONS FALLEN OVER LARGE BASINS HYDROLOGICAL PURPOSES INSTANCE RIVER FLOOD CONTROL SEWER MANAGEMENT CONSTRUCTION AREAS WHERE PLANNERS RAINFALL ACCUMULATION DATA RADAR-DERIVED RAINFALL ESTIMATES COMPLIMENT SURFACE STATION DATA WHICH USED CALIBRATION PRODUCE RADAR ACCUMULATIONS RAIN RATES OVER POINT ESTIMATED USING VALUE REFLECTIVITY DATA INDIVIDUAL GRID POINTS RADAR EQUATION THEN USED WHICH DISPLAYSTYLE WHERE REPRESENTS RADAR REFLECTIVITY REPRESENTS RAINFALL RATE CONSTANTS SATELLITE DERIVED RAINFALL ESTIMATES PASSIVE MICROWAVE INSTRUMENTS ABOARD POLAR ORBITING WELL GEOSTATIONARY WEATHER SATELLITES INDIRECTLY MEASURE RAINFALL RATES WANTS ACCUMULATED RAINFALL OVER TIME PERIOD ACCUMULATIONS FROM EACH GRID WITHIN IMAGES DURING THAT TIME FILE RAIN RAIN HEAVIEST RAIN SEEN REDS YELLOWS FILE RAIN RAIN INTENSITY HEAVY RAIN GLENSHAW PENNSYLVANIA MENU SOUND HEAVY RAIN FALL SUBURBAN NEIGHBORHOOD PROBLEMS PLAYING THIS FILE MEDIA HELP RAINFALL INTENSITY CLASSIFIED ACCORDING RATE PRECIPITATION LIGHT RAIN WHEN PRECIPITATION RATE HOUR MODERATE RAIN WHEN PRECIPITATION RATE BETWEEN HOUR HEAVY RAIN WHEN PRECIPITATION RATE HOUR BETWEEN HOUR VIOLENT RAIN WHEN PRECIPITATION RATE HOUR EUPHEMISMS HEAVY VIOLENT RAIN INCLUDE GULLY WASHER TRASH-MOVER TOAD-STRANGLER INTENSITY ALSO EXPRESSED RAINFALL EROSIVITY R-FACTOR RETURN PERIOD ALSO -YEAR FLOOD LIKELIHOOD PROBABILITY EVENT WITH SPECIFIED INTENSITY DURATION CALLED RETURN PERIOD FREQUENCY INTENSITY STORM PREDICTED RETURN PERIOD STORM DURATION FROM CHARTS BASED HISTORIC DATA LOCATION TERM YEAR STORM DESCRIBES RAINFALL EVENT WHICH RARE ONLY LIKELY OCCUR ONCE EVERY YEARS PERCENT LIKELIHOOD GIVEN YEAR RAINFALL WILL GREATER FLOODING WILL WORSE THAN WORST STORM EXPECTED SINGLE YEAR TERM YEAR STORM DESCRIBES RAINFALL EVENT WHICH EXTREMELY RARE WHICH WILL OCCUR WITH LIKELIHOOD ONLY ONCE CENTURY PERCENT LIKELIHOOD GIVEN YEAR RAINFALL WILL EXTREME FLOODING WORSE THAN YEAR EVENT WITH PROBABILITY EVENTS POSSIBLE THOUGH IMPROBABLE HAVE MULTIPLE YEAR STORMS SINGLE YEAR FORECASTING MAIN ARTICLE QUANTITATIVE PRECIPITATION FORECAST EXAMPLE FIVE-DAY RAINFALL FORECAST FROM HYDROMETEOROLOGICAL PREDICTION CENTER QUANTITATIVE PRECIPITATION FORECAST ABBREVIATED EXPECTED AMOUNT LIQUID PRECIPITATION ACCUMULATED OVER SPECIFIED TIME PERIOD OVER SPECIFIED AREA WILL SPECIFIED WHEN MEASURABLE PRECIPITATION TYPE REACHING MINIMUM THRESHOLD FORECAST HOUR DURING VALID PERIOD PRECIPITATION FORECASTS TEND BOUND SYNOPTIC HOURS SUCH TERRAIN CONSIDERED QPFS TOPOGRAPHY BASED UPON CLIMATOLOGICAL PRECIPITATION PATTERNS FROM OBSERVATIONS WITH FINE DETAIL STARTING LATE QPFS WERE USED WITHIN HYDROLOGIC FORECAST MODELS SIMULATE IMPACT RIVERS THROUGHOUT UNITED STATES FORECAST MODELS SHOW SIGNIFICANT SENSITIVITY HUMIDITY LEVELS WITHIN PLANETARY BOUNDARY LAYER LOWEST LEVELS ATMOSPHERE WHICH DECREASES WITH HEIGHT GENERATED QUANTITATIVE FORECASTING AMOUNTS QUALITATIVE FORECASTING PROBABILITY SPECIFIC AMOUNT BASIS RADAR IMAGERY FORECASTING TECHNIQUES SHOW HIGHER SKILL THAN MODEL FORECASTS WITHIN HOURS TIME RADAR IMAGE FORECASTS VERIFIED THROUGH RAIN GAUGE MEASUREMENTS WEATHER RADAR ESTIMATES COMBINATION BOTH VARIOUS SKILL SCORES DETERMINED MEASURE VALUE RAINFALL FORECAST IMPACT EFFECT AGRICULTURE RAINFALL ESTIMATES SOUTHERN JAPAN SURROUNDING REGION FROM JULY PRECIPITATION ESPECIALLY RAIN DRAMATIC EFFECT AGRICULTURE PLANTS NEED LEAST SOME WATER SURVIVE THEREFORE RAIN BEING MOST EFFECTIVE MEANS WATERING IMPORTANT AGRICULTURE WHILE REGULAR RAIN PATTERN USUALLY VITAL HEALTHY PLANTS MUCH LITTLE RAINFALL HARMFUL EVEN DEVASTATING CROPS DROUGHT KILL CROPS INCREASE EROSION WHILE OVERLY WEATHER CAUSE HARMFUL FUNGUS GROWTH PLANTS NEED VARYING AMOUNTS RAINFALL SURVIVE EXAMPLE CERTAIN CACTI REQUIRE SMALL AMOUNTS WATER WHILE TROPICAL PLANTS NEED HUNDREDS INCHES RAIN YEAR SURVIVE AREAS WITH SEASONS SOIL NUTRIENTS DIMINISH EROSION INCREASES DURING SEASON ANIMALS HAVE ADAPTATION SURVIVAL STRATEGIES WETTER REGIME PREVIOUS SEASON LEADS FOOD SHORTAGES INTO SEASON CROPS HAVE MATURE DEVELOPING COUNTRIES HAVE NOTED THAT THEIR POPULATIONS SHOW SEASONAL WEIGHT FLUCTUATIONS FOOD SHORTAGES SEEN BEFORE FIRST HARVEST WHICH OCCURS LATE SEASON RAIN HARVESTED THROUGH RAINWATER TANKS TREATED POTABLE NON-POTABLE INDOORS IRRIGATION EXCESSIVE RAIN DURING SHORT PERIODS TIME CAUSE FLASH FLOODS CULTURE ALSO LIST RAIN DEITIES CULTURAL ATTITUDES TOWARDS RAIN DIFFER ACROSS WORLD TEMPERATE CLIMATES PEOPLE TEND MORE STRESSED WHEN WEATHER UNSTABLE CLOUDY WITH IMPACT GREATER THAN WOMEN RAIN ALSO BRING SOME CONSIDER SOOTHING ENJOY AESTHETIC APPEAL PLACES SUCH INDIA DURING PERIODS DROUGHT RAIN LIFTS PEOPLE'S MOODS BOTSWANA SETSWANA WORD RAIN PULA USED NAME NATIONAL CURRENCY RECOGNITION ECONOMIC IMPORTANCE RAIN THIS DESERT COUNTRY SEVERAL CULTURES HAVE DEVELOPED MEANS DEALING WITH RAIN HAVE DEVELOPED NUMEROUS PROTECTION DEVICES SUCH UMBRELLAS RAINCOATS DIVERSION DEVICES SUCH GUTTERS STORM DRAINS THAT LEAD RAINS SEWERS MANY PEOPLE FIND SCENT DURING IMMEDIATELY AFTER RAIN PLEASANT DISTINCTIVE SOURCE THIS SCENT PETRICHOR PRODUCED PLANTS THEN ABSORBED ROCKS SOIL LATER RELEASED INTO DURING RAINFALL GLOBAL CLIMATOLOGY ALSO EARTH RAINFALL CLIMATOLOGY APPROXIMATELY WATER FALLS PRECIPITATION EACH YEAR ACROSS GLOBE WITH OVER OCEANS GIVEN EARTH'S SURFACE AREA THAT MEANS GLOBALLY AVERAGED ANNUAL PRECIPITATION DESERTS DEFINED AREAS WITH AVERAGE ANNUAL PRECIPITATION LESS THAN YEAR AREAS WHERE MORE WATER LOST EVAPOTRANSPIRATION THAN FALLS PRECIPITATION DESERTS MAIN ARTICLE DESERT LARGEST DESERTS NORTHERN HALF AFRICA OCCUPIED WORLD'S MOST EXTENSIVE REGION SAHARA DESERT SOME DESERTS ALSO OCCUPYING MUCH SOUTHERN AFRICA NAMIB KALAHARI ACROSS ASIA LARGE ANNUAL RAINFALL MINIMUM COMPOSED PRIMARILY DESERTS STRETCHES FROM GOBI DESERT MONGOLIA WEST-SOUTHWEST THROUGH WESTERN PAKISTAN BALOCHISTAN IRAN INTO ARABIAN DESERT SAUDI ARABIA MOST AUSTRALIA SEMI-ARID DESERT MAKING WORLD'S DRIEST INHABITED CONTINENT SOUTH AMERICA ANDES MOUNTAIN RANGE BLOCKS PACIFIC MOISTURE THAT ARRIVES THAT CONTINENT RESULTING DESERTLIKE CLIMATE JUST DOWNWIND ACROSS WESTERN ARGENTINA DRIER AREAS DESKOV ääNSISH AIKSETKä VERäISESA KANTI JOUžNOJVOJA YLISSAALLYSTAA AIKISäSLOVAKKO LäNTYVIN HORTEE OPISTOR PUODIFORISH DOBNýCH KIEN ALTTIO MUUTTAIKSEN KIRJAT NIMBURóPSKEET JONANSONKAAN VIRYHYT BULOVEDNý 'ASTAA MURTERBI DIFTONE POLAALA KUIVU WHAT NEXT
Thanks to úDARMS TOISH for these words.
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- Another batch of random words from this seed set.
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