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Seed Words for Rain

KYUNG TANG AATU SHIN JUKU CHIKE HASIB CHANG CHéNG CHéNG- GONG CHóNG CONG DàWEI DàZHONG DéHUá DéSHèNG LOGIN REGISTER SEARCH NAMESMEANINGSPOPULARITIESNAMESAKESNAME DAYSRELATED NAMESGLOSSARY SADERAIN FROM WIKIPEDIA FREE ENCYCLOPEDIA THIS LATEST ACCEPTED REVISION ACCEPTED SEPTEMBER JUMP NAVIGATION SEARCH THIS ARTICLE ABOUT PRECIPITATION OTHER USES RAIN DISAMBIGUATION RAINY REDIRECTS HERE OTHER USES RAINY DISAMBIGUATION RAIN SHAFT BASE THUNDERSTORMRAIN LIQUID PRECIPITATION OPPOSED NON-LIQUID KINDS PRECIPITATION SUCH SNOW HAIL SLEET RAIN REQUIRES PRESENCE THICK LAYER ATMOSPHERE HAVE TEMPERATURES ABOVE MELTING POINT WATER NEAR ABOVE EARTH'S SURFACE EARTH CONDENSATION ATMOSPHERIC WATER VAPOR INTO DROPS WATER HEAVY ENOUGH FALL OFTEN MAKING SURFACE PROCESSES POSSIBLY ACTING TOGETHER LEAD BECOMING SATURATED LEADING RAINFALL COOLING ADDING WATER VAPOR VIRGA PRECIPITATION THAT BEGINS FALLING EARTH EVAPORATES BEFORE REACHING SURFACE WAYS BECOME SATURATED PRECIPITATION FORMS COLLISION WITH OTHER RAIN DROPS CRYSTALS WITHIN CLOUD RAIN DROPS RANGE SIZE FROM OBLATE PANCAKE-LIKE SHAPES LARGER DROPS SMALL SPHERES SMALLER DROPS MOISTURE MOVING ALONG THREE-DIMENSIONAL ZONES TEMPERATURE MOISTURE CONTRASTS KNOWN WEATHER FRONTS MAJOR METHOD RAIN PRODUCTION ENOUGH MOISTURE UPWARD MOTION PRESENT PRECIPITATION FALLS FROM CONVECTIVE CLOUDS THOSE WITH STRONG UPWARD VERTICAL MOTION SUCH CUMULONIMBUS THUNDERSTORMS 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 RAIN PRIMARY SOURCE FRESHWATER MOST AREAS WORLD PROVIDING SUITABLE CONDITIONS DIVERSE ECOSYSTEMS WELL WATER HYDROELECTRIC POWER PLANTS CROP IRRIGATION RAINFALL MEASURED THROUGH RAIN GAUGES RAINFALL AMOUNTS ESTIMATED ACTIVELY WEATHER RADAR PASSIVELY WEATHER SATELLITES 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 PRECIPITATION MAJOR COMPONENT WATER CYCLE RESPONSIBLE DEPOSITING MOST FRESH WATER PLANET GLOBALLY-AVERAGED ANNUAL PRECIPITATION MILLIMETRES CLIMATE CLASSIFICATION SYSTEMS SUCH KöPPEN CLIMATE CLASSIFICATION SYSTEM AVERAGE ANNUAL RAINFALL HELP DIFFERENTIATE BETWEEN DIFFERING CLIMATE REGIMES ANTARCTICA EARTH'S DRIEST CONTINENT RAIN ALSO KNOWN SUSPECTED OTHER WORLDS COMPOSED METHANE IRON NEON SULFURIC ACID RATHER THAN WATER PART NATURE SERIES WEATHER CALENDAR SEASONS SPRING SUMMER AUTUMN WINTER TROPICAL SEASONS SEASON SEASON STORMS THUNDERSTORM SUPERCELL DOWNBURST LIGHTNING TORNADO WATERSPOUT TROPICAL CYCLONE HURRICANE EXTRATROPICAL CYCLONE WINTER STORM BLIZZARD STORM DUST STORM FIRESTORM CLOUD PRECIPITATION DRIZZLE RAIN SNOW GRAUPEL FREEZING RAIN PELLETS HAIL TOPICS METEOROLOGY CLIMATE WEATHER FORECASTING HEAT WAVE POLLUTION WEATHER PORTAL CONTENTS HIDE FORMATION WATER-SATURATED COALESCENCE 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 WETLANDS IMPACT WESTERLIES WETTEST KNOWN LOCATIONS OUTSIDE EARTH ALSO NOTES REFERENCES EXTERNAL LINKS EDIT FORMATION EDIT WATER-SATURATED CLOUDS FORM RESPONSE COLD FRONTAIR 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 EDIT COALESCENCE SHAPE RAIN DROPS DEPEND UPON THEIR SIZECOALESCENCE OCCURS WHEN WATER DROPLETS FUSE CREATE LARGER WATER DROPLETS WHEN WATER DROPLETS FREEZE ONTO CRYSTAL WHICH KNOWN BERGERON PROCESS 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 MILLIMETRES MILLIMETRES 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 MILLIMETRES LARGE SIZE EXPLAINED CONDENSATION LARGE SMOKE PARTICLES COLLISIONS BETWEEN DROPS SMALL REGIONS WITH PARTICULARLY HIGH CONTENT LIQUID WATER INTENSITY DURATION RAINFALL USUALLY INVERSELY RELATED HIGH INTENSITY STORMS LIKELY SHORT DURATION INTENSITY STORMS HAVE LONG DURATION RAIN DROPS ASSOCIATED WITH MELTING HAIL TEND LARGER THAN OTHER RAIN DROPS RAINDROPS IMPACT THEIR TERMINAL VELOCITY WHICH GREATER LARGER DROPS THEIR LARGER MASS DRAG RATIO LEVEL WITHOUT WIND MILLIMETRES DRIZZLE IMPACTS METRES SECOND WHILE LARGE MILLIMETRES DROPS IMPACT AROUND METRES SECOND SOUND RAINDROPS HITTING WATER CAUSED BUBBLES OSCILLATING UNDERWATER METAR CODE RAIN WHILE CODING RAIN SHOWERS SHRA EDIT CAUSES EDIT 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 FEET ABOVE GROUND LEVEL EDIT CONVECTION CONVECTIVE PRECIPITATIONCONVECTIVE 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 EDIT OROGRAPHIC EFFECTS MAIN ARTICLES OROGRAPHIC LIFT PRECIPITATION TYPES METEOROLOGY UNITED STATES RAINFALL CLIMATOLOGY OROGRAPHIC PRECIPITATIONOROGRAPHIC 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 INCHES 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 EDIT WITHIN TROPICS RAINFALL DISTRIBUTION MONTH CAIRNS SHOWING EXTENT SEASON THAT LOCATIONSEE 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 EDIT HUMAN INFLUENCE IMAGE ATLANTA GEORGIA SHOWING TEMPERATURE DISTRIBUTION WITH BLUE SHOWING COOL TEMPERATURES WARM AREAS APPEAR WHITE 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 MILES MILES DOWNWIND CITIES COMPARED WITH UPWIND SOME CITIES INDUCE TOTAL PRECIPITATION INCREASE MEAN SURFACE TEMPERATURE ANOMALIES DURING PERIOD WITH RESPECT AVERAGE TEMPERATURES FROM 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 CENTURY SINCE WITH GREATEST INCREASES WITHIN EAST NORTH CENTRAL CLIMATE REGION PERCENT CENTURY SOUTH PERCENT HAWAII ONLY REGION SHOW DECREASE PERCENT MOST SUCCESSFUL ATTEMPTS INFLUENCING WEATHER INVOLVE CLOUD SEEDING WHICH INCLUDE TECHNIQUES USED INCREASE WINTER PRECIPITATION OVER MOUNTAINS SUPPRESS HAIL EDIT CHARACTERISTICS EDIT PATTERNS BAND THUNDERSTORMS SEEN WEATHER RADAR DISPLAYMAIN 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 EDIT ACIDITY ALSO ACID RAIN RAINFALL WITH LEVELS ALSO KNOWN ACID RAIN PRODUCED LIGHTNING WITHIN THUNDERSTORMS FREQUENT RISK LIQUIDS WITH LEVELS LESS THAN ACIDS THOSE WITH LEVELS GREATER THAN BASES DISTILLED WATER WHICH ABOUT FORM CARBONIC ACID YELLOWISH TINT DISTILLED WATER WITH CARBON DIOXIDE REMOVED NEUTRAL “CLEAN” UNPOLLUTED RAIN SLIGHTLY ACIDIC ABOUT UNPOLLUTED RAIN ALSO CONTAINS OTHER CHEMICALS NITROUS OXIDE PRESENT DURING THUNDERSTORM PHENOMENA CAUSED SPLITTING NITROGEN MOLECULES RESULT PRODUCTION ACID RAIN COMBINES WITH WATER MOLECULES DURING PRECIPITATION NITRIC OXIDE PRESENT ATMOSPHERE PRODUCED INTERNAL COMBUSTION ENGINES SULFUR DIOXIDE INTRODUCED RAINFALL THROUGH EXPULSION VOLCANIC GASES PRODUCT FOSSIL FUEL COMBUSTION TURNING RAINFALL INTO SULFURIC ACID LIVESTOCK PRODUCTION RESPONSIBLE ALMOST TWO-THIRDS ANTHROPOGENIC SOURCES AMMONIA WHICH CONTRIBUTES SIGNIFICANTLY ACID RAIN ACID RAIN DAMAGE BUILDINGS OTHER EXTERNAL STRUCTURES ECOSYSTEMS ACID RAIN CAUSE DEATHS PLANTS MARINE LIFE INCREASING ACIDITY SOIL BODIES WATER EDIT 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 MILLIMETRES MILLIMETRES TROPICAL SAVANNA GRASSLANDBIOME LOCATED SEMI-ARID SEMI-HUMID CLIMATE REGIONS SUBTROPICAL TROPICAL LATITUDES WITH RAINFALL BETWEEN MILLIMETRES MILLIMETRES 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 EDIT MEASUREMENT EDIT GAUGES STANDARD RAIN GAUGESEE ALSO RAIN GAUGE DISDROMETER SNOW GAUGE STANDARD MEASURING RAINFALL SNOWFALL STANDARD RAIN GAUGE WHICH FOUND PLASTIC METAL VARIETIES INNER CYLINDER FILLED RAIN WITH OVERFLOW FLOWING INTO OUTER CYLINDER PLASTIC GAGES 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 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 MILLIMETER RAINFALL EQUIVALENT LITER WATER SQUARE METER THIS MAKES COMPUTING WATER REQUIREMENTS CROPS SIMPLE EDIT 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 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 EDIT INTENSITY HEAVY RAIN GLENSHAW SOUND HEAVY RAIN FALL SUBURBAN NEIGHBORHOOD -------------------------------------------------------------------------------- PROBLEMS LISTENING THIS FILE MEDIA HELP RAINFALL INTENSITY CLASSIFIED ACCORDING RATE PRECIPITATION LIGHT RAIN WHEN PRECIPITATION RATE MILLIMETRES HOUR MODERATE RAIN WHEN PRECIPITATION RATE BETWEEN MILLIMETRES MILLIMETRES MILLIMETRES HOUR HEAVY 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MERIDIAN MOUNTAINS PACIFIC NORTHWEST SIERRA NEVADA RANGE WETTER PORTIONS NATION WITH AVERAGE RAINFALL EXCEEDING INCHES YEAR TROPICAL CYCLONES ENHANCE PRECIPITATION ACROSS SOUTHERN SECTIONS UNITED STATES WELL PUERTO RICO UNITED STATES VIRGIN ISLANDS NORTHERN MARIANA ISLANDS GUAM AMERICAN SAMOA EDIT IMPACT WESTERLIES LONG-TERM MEAN PRECIPITATION MONTHSEE ALSO WESTERLIES WESTERLY FLOW FROM MILD NORTH ATLANTIC LEADS WETNESS ACROSS WESTERN EUROPE PARTICULAR UNITED KINGDOM WHERE WESTERN COASTS RECEIVE BETWEEN SEA-LEVEL MOUNTAINS RAIN YEAR BERGEN NORWAY MORE FAMOUS EUROPEAN RAIN-CITIES WITH YEARLY PRECIPITATION AVERAGE DURING FALL WINTER SPRING PACIFIC STORM SYSTEMS BRING MOST HAWAII WESTERN UNITED STATES MUCH THEIR PRECIPITATION OVER RIDGE STREAM BRINGS SUMMER PRECIPITATION MAXIMUM GREAT LAKES LARGE THUNDERSTORM AREAS KNOWN MESOSCALE CONVECTIVE COMPLEXES MOVE THROUGH PLAINS MIDWEST GREAT LAKES DURING WARM SEASON CONTRIBUTING ANNUAL PRECIPITATION REGION NIñO-SOUTHERN OSCILLATION AFFECTS 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MAWSYNRAM INDIA HIGHEST YEAR ASIA CHERRAPUNJI INDIA HIGHEST CALENDAR MONTH ASIA CHERRAPUNJI INDIA HIGHEST HOURS INDIAN OCEAN REUNION ISLAND HIGHEST HOURS INDIAN OCEAN BELOUVE REUNION ISLAND HIGHEST MINUTE NORTH AMERICA GUADELOUPE CARIBBEAN ISLANDS EDIT OUTSIDE EARTH TITAN SATURN'S LARGEST MOON INFREQUENT METHANE RAIN THOUGHT CARVE MOON'S NUMEROUS SURFACE CHANNELS VENUS SULFURIC ACID VIRGA EVAPORATES KILOMETRES FROM SURFACE THERE LIKELY RAIN VARIOUS COMPOSITIONS UPPER ATMOSPHERES GIANTS WELL PRECIPITATION LIQUID NEON DEEP ATMOSPHERES EXTRASOLAR PLANET OGLE-TR- CONSTELLATION SAGITTARIUS REPORTED HAVE IRON RAIN EDIT ALSO JOHAD RAIN DANCING RAIN SENSOR RAINBOW RAINING ANIMALS RAIN KERALA SANITARY SEWER OVERFLOW SEDIMENT PRECIPITATION WATER RESOURCES WEATHER EDIT NOTES VALUE GIVEN CONTINENT'S HIGHEST POSSIBLY WORLD'S DEPENDING MEASUREMENT PRACTICES PROCEDURES PERIOD RECORD VARIATIONS OFFICIAL GREATEST AVERAGE ANNUAL PRECIPITATION SOUTH AMERICA INCHES QUIBDO COLOMBIA INCHES AVERAGE LLORO 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ALLENPRESS GLOSSARY SEARCH ADIABATIC-PROCESS RETRIEVED TECHNOLOGY PELTIER COLD PLATE HTTP TETECH COLD-PLATE-COOLERS HTML RETRIEVED GLOSSARY METEOROLOGY RADIATIONAL COOLING AMERICAN METEOROLOGICAL SOCIETY HTTP AMSGLOSSARY ALLENPRESS GLOSSARY SEARCH QUERY RADIATIONAL COOLING SUBMIT SEARCH RETRIEVED ROBERT FOVELL APPROACHES SATURATION UNIVERSITY CALIFORNIA ANGELESE HTTP ATMOS UCLA FOVELL DOWNLOADS SATURATION RETRIEVED ROBERT PENROSE PEARCE METEOROLOGY MILLENNIUM ACADEMIC PRESS ISBN HTTP BOOKS GOOGLE QECY UBDYRCC WAYS MOISTEN ATMOSPHERE RETRIEVED NATIONAL WEATHER SERVICE OFFICE SPOKANE WASHINGTON VIRGA THUNDERSTORMS HTTP NOAA OUTREACH TTALK VIRGA RETRIEVED BART HURK ELEANOR BLYTH GLOBAL MAPS LOCAL LAND-ATMOSPHERE COUPLING KNMI HTTP KNMI HURKVD LOCO WORKSHOP WORKSHOP REPORT RETRIEVED KRISHNA RAMANUJAN BRAD BOHLANDER LANDCOVER CHANGES RIVAL GREENHOUSE GASES CAUSE CLIMATE CHANGE NATIONAL AERONAUTICS SPACE ADMINISTRATION GODDARD SPACE FLIGHT CENTER ARCHIVED FROM ORIGINAL JUNE HTTP ARCHIVE HTTP GSFC NASA TOPSTORY LANDCOVER HTML RETRIEVED NATIONAL WEATHER SERVICE JETSTREAM MASSES HTTP WEATHER JETSTREAM SYNOPTIC AIRMASS RETRIEVED MICHAEL PIDWIRNY CHAPTER INTRODUCTION HYDROSPHERE CLOUD FORMATION PROCESSES PHYSICAL GEOGRAPHY HTTP PHYSICALGEOGRAPHY FUNDAMENTALS HTML RETRIEVED GLOSSARY METEOROLOGY JUNE FRONT AMERICAN METEOROLOGICAL SOCIETY HTTP AMSGLOSSARY ALLENPRESS GLOSSARY SEARCH FRONT RETRIEVED DAVID ROTH UNIFIED SURFACE ANALYSIS MANUAL HYDROMETEOROLOGICAL PREDICTION CENTER HTTP NCEP NOAA UASFCMANUALVERSION RETRIEVED STRATUS METEOROLOGICAL PHYSICAL BACKGROUND ZENTRALANSTALT METEOROLOGIE GEODYNAMIK HTTP ZAMG DOCU MANUAL SATMANU MAIN DOCU MANUAL SATMANU FGSTR BACKGR RETRIEVED GLOSSARY METEOROLOGY JUNE WARM RAIN PROCESS AMERICAN METEOROLOGICAL SOCIETY HTTP AMSGLOSSARY ALLENPRESS GLOSSARY SEARCH WARM-RAIN-PROCESS RETRIEVED PAUL SIRVATKA CLOUD PHYSICS COLLISION COALESCENCE BERGERON PROCESS COLLEGE DUPAGE HTTP WEATHER SIRVATKA BERGERON HTML RETRIEVED ALISTAIR FRASER METEOROLOGY RAINDROPS SHAPED LIKE TEARDROPS PENNSYLVANIA STATE UNIVERSITY HTTP FRASER BADRAIN HTML RETRIEVED UNITED STATES GEOLOGICAL SURVEY RAINDROPS TEAR SHAPED UNITED STATES DEPARTMENT INTERIOR HTTP WATER USGS RAINDROPSHAPE HTML RETRIEVED PAUL RINCON MONSTER RAINDROPS DELIGHT EXPERTS BRITISH BROADCASTING COMPANY HTTP NEWS SCIENCE NATURE RETRIEVED GUNTOYINBO AKINTOLA RAINSTORM CHARACTERISTICS AFFECTING WATER AVAILABILITY AGRICULTURE IAHS PUBLICATION NUMBER HTTP ENSMP IAHS REDBOOKS IAHS RETRIEVED ROBERT HOUZE OCTOBER STRATIFORM PRECIPITATION REGIONS CONVECTION METEOROLOGICAL PARADOX BULLETIN AMERICAN METEOROLOGICAL SOCIETY SPIROC HTTP ALLENPRESS ARCHIVE RETRIEVED DEAD LINK NORMAN JUNKER INGREDIENTS BASED METHODOLOGY FORECASTING PRECIPITATION ASSOCIATED WITH MCS’S HYDROMETEOROLOGICAL PREDICTION CENTER HTTP NCEP NOAA RESEARCH TEST TEST FILES PAGE RETRIEVED FALLING RAINDROPS SPEEDS WEATHER QUEST HTTP WONDERQUEST FALLING-RAINDROPS RETRIEVED ANDREA PROSPERETTI HASAN OGUZ IMPACT DROPS LIQUID SURFACES 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SUBMIT SEARCH RETRIEVED TOBY CARLSON MID-LATITUDE WEATHER SYSTEMS ROUTLEDGE ISBN HTTP BOOKS GOOGLE LIVAAAAIAAJ WHERE CONVECTION OCCURS MID-LATITUDES RETRIEVED DIANA LEONE RAIN SUPREME HONOLULU STAR-BULLETIN HTTP STARBULLETIN NEWS STORY HTML RETRIEVED STEVEN BUSINGER THOMAS BIRCHARD ECHO SEVERE WEATHER ASSOCIATED WITH KONA HAWAII RETRIEVED WESTERN REGIONAL CLIMATE CENTER CLIMATE HAWAII HTTP WRCC NARRATIVES HAWAII RETRIEVED PAUL LYDOLPH CLIMATE EARTH ROWMAN LITTLEFIELD ISBN HTTP BOOKS GOOGLE BBJIUXHEGZ EFFECT ANDES RAINFALL CHILE RETRIEVED MICHAEL MARES ENCYCLOPEDIA DESERTS UNIVERSITY OKLAHOMA PRESS ISBN HTTP BOOKS GOOGLE CBQZTAF SIERRA NEVADA LEADS GREAT BASIN DESERT RETRIEVED ADAM GANSON GEOLOGY DEATH VALLEY INDIANA UNIVERSITY HTTP INDIANA SIERRA PAPERS GANSON HTML RETRIEVED GLOSSARY METEOROLOGY RAINY SEASON AMERICAN METEOROLOGICAL SOCIETY HTTP AMSGLOSSARY ALLENPRESS GLOSSARY SEARCH RAINY-SEASON RETRIEVED COSTA RICA GUIDE WHEN TRAVEL COSTA RICA TOUCANGUIDES HTTP COSTA-RICA-GUIDE WHEN RETRIEVED MICHAEL PIDWIRNY CHAPTER INTRODUCTION BIOSPHERE PHYSICALGEOGRAPHY HTTP PHYSICALGEOGRAPHY FUNDAMENTALS HTML RETRIEVED ELISABETH BENDERS-HYDE WORLD CLIMATES BLUE PLANET BIOMES HTTP BLUEPLANETBIOMES CLIMATE RETRIEVED ZHENG SOURCES CHARACTERISTICS ATMOSPHERIC PARTICULATES DURING SEASONS HONG KONG UNIVERSITY RHODE ISLAND HTTP DIGITALCOMMONS DISSERTATIONS RETRIEVED OGBAN HORSFALL AKPORHONOR SEASONAL VARIATIONS PHYSICO-CHEMICAL CHARACTERISTICS WATER RESOURCES QUALITY WESTERN NIGER DELTA REGION NIGERIA JOURNAL APPLIED SCIENTIFIC ENVIRONMENTAL MANAGEMENT ISSN HTTPS TSPACE LIBRARY UTORONTO BITSTREAM RETRIEVED HAYNES RIDPATH WILLIAMS MONSOONAL AUSTRALIA TAYLOR FRANCIS ISBN HTTP BOOKS GOOGLE ZHVTSMJYUN SEASON CHARACTERISTICS RETRIEVED CHRIS LANDSEA SUBJECT TROPICAL CYCLONES' WINDS ROTATE COUNTER-CLOCKWISE CLOCKWISE NORTHERN SOUTHERN HEMISPHERE NATIONAL HURRICANE CENTER HTTP AOML NOAA TCFAQ HTML RETRIEVED CLIMATE PREDICTION CENTER TROPICAL EASTERN NORTH PACIFIC HURRICANE OUTLOOK NATIONAL OCEANIC ATMOSPHERIC ADMINISTRATION HTTP NCEP NOAA PRODUCTS EPAC HURR EPAC HURRICANE HTML RETRIEVED JACK WILLIAMS BACKGROUND CALIFORNIA'S TROPICAL STORMS TODAY HTTP USATODAY WEATHER WHHCALIF RETRIEVED CERVENY BALLING WEEKLY CYCLES POLLUTANTS PRECIPITATION TROPICAL CYCLONES COASTAL ATLANTIC REGION NATURE DALE FUCHS SPAIN GOES HI-TECH BEAT DROUGHT LONDON GUARDIAN HTTP GUARDIAN WEATHER STORY HTML RETRIEVED GODDARD SPACE FLIGHT CENTER NASA SATELLITE CONFIRMS URBAN HEAT ISLANDS INCREASE RAINFALL AROUND CITIES NATIONAL AERONAUTICS SPACE ADMINISTRATION ARCHIVED FROM ORIGINAL JUNE HTTP ARCHIVE HTTP GSFC NASA TOPSTORY URBANRAIN HTML RETRIEVED CLIMATE CHANGE DIVISION PRECIPITATION STORM CHANGES UNITED STATES ENVIRONMENTAL PROTECTION AGENCY HTTP CLIMATECHANGE SCIENCE RECENTPSC HTML RETRIEVED AMERICAN METEOROLOGICAL SOCIETY PLANNED INADVERTENT WEATHER MODIFICATION HTTP AMETSOC POLICY WXMOD HTML RETRIEVED GLOSSARY METEOROLOGY RAINBAND RETRIEVED GLOSSARY METEOROLOGY BANDED STRUCTURE RETRIEVED OWEN 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DAMIANO DAMIANOS DAMIANUS DAMIEN DAMIJAN DAMION DAMIR DAMJAN DAMOCLES DAMODAR DAMODARA DAMON DAMYAN DANA DANAIL DAND DANE DANEL DANI DÁNIEL DANIËL DANIEL DANIELE DANIELIUS DANIHEL DANIIL DANIILU DANIJEL DANILO DANIYYEL DANNIE DANNY DANTE DAQUAN DARA DARA DARA DARACH DARAGH DARAYAVAHUSH DARBY DARCY DARDAN DARDANOS DARDEN DAREIOS DARELL DAREN DARIAN DARIEN DARIJO DARIJUS DARIN DARÍO DARIO DARION DARIUS DARIUSH DARIUSZ DARKO DARMA DARNELL DARRAGH DARREL DARRELL DARREN DARRIN DARRYL D'ARTAGNAN DARWIN DARYAWESH DARYL DARYUSH DASHIELL DATHAN DAUD DAUID DAVE DAVETH DAVEY DAVI DÁVID DAVID DAVIDE DAVIDU DAVIE DAVIN DAVIS DAVOR DAVY DAWID DAWOOD DAWSON DAWUD DAYARAM DAYTON DAZBOG DAZHDBOG DEACON DEAN DEANDRE DEANGELO DEASÚN DEBDAN DECEBAL DECIMUS DECLAN DEDRICK DEEMER DEEPAK DEFOREST DEFORREST DEIMOS DEINIOL DEION DEJAN DEKEL DELAIAH DELANO DELAYAHU DELBERT DELL DELMAR DELPHINUS DELROY DELSHAD DELWYN DEMETER DEMÉTRIO DEMETRIO DEMETRIOS DEMETRIUS DEMOCRITUS DEMON DEMOSTHENES DEMYAN DENE DENEB DÉNES DENHOLM DENIEL DENIS DENNIS DENNY DENTON DENVER DENYS DENZEL DENZIL DEODAN DÉODAT DEODATUS DEON DEONTE DEÒRSA DERBY DEREK DERICK DERMID DERMOT DEROR DERREN DERRICK DERRY DERRYL DERYA DERYCK DESHAUN DESHAWN DESI DESIDERATUS DESIDÉRIO DESIDERIO DESIDERIUS DÉSIRÉ DESISLAV DESMOND DESTA DESYA DETLEF DEUSDEDIT DEVADAS DEVAN DEVARAJA DEVDAN DEVDAS DEVEN DEVEREUX DEVIN DEVON DEVRAJ DEVR DEVYN DEWAYNE DEWEY DEWI DEWYDD DEXTER DEYAN DEZI DEZS DHANANJAY DHAVAL DIAN DIARMAD DIARMAID DIARMUID DICK DICK DÍDAC DIDACUS DIDI DIDIER DIEDE DIEDERICH DIEDERICK DIEDERIK DIEGO DIERK DIETER DIETFRIED DIETHELM DIETMAR DIETRICH DIEUDONNÉ DIEUWE DIGBY DIGGORY DIKLA DIKLAH DILBERT DILIP DILIPA DILLON DILSHAD DILWYN DIMA DIMAS DIMITAR DIMITRI D

Thanks to DIES DORM for these words.

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