CLASS NOTES Flashcards
LAPSE TRIBE
FINLAND
SAMOYEDS
SIBERIA
POLAR TYPE OF CLIMATE
TUNDRRA
NE NORTH AMERICA AND NE ASIA
LAURENTIAN
COLD POLE OF WORLD
SIBERIAN
NORTH WEST EUROPE MARITIME/
BRITISH TYPE
WARM WESTERLIES THROUGHOUT THE YEAR
BRITISH
TEMPERATE OR PSEUDO MONSOON CLIMATE
CHINA TYPE
ONSHORE WIND CONDITIONS
HIGH TEMPERATURE
LOW PRESSURE
TEMPERATE MONSOON CLIMATE/
PSEUDO CLIMATE
LATITUDE OF TORANDOES
MID LATITUDE
SMALL DIAMETER COLUMN OF VIOLENTLY ROTATING AIR DEVELOPED WITHIN A CONVECTIVE CLOUD AND IN CONTACT WITH THE GROUND
TORANDOES
STRONGEST WIND KNOWN ON THE EARTH
TORANDOES
TORANDOES OCCUR IN
LAND OR SEA
TORANDOES ON SEA
WATER SPROUT
TORANDO SPEED
500 KM
300 MILES
WHEN GROUND GETS HEATED FOG—-
LIFTS UP
FOG OCCURS IN
EARLY MORNING
REASON FOR FOG
RADIATIVE COOLING
NORTH OF TROPIC OF CANCER
WESTERLIES
MID LATITUDE STORM OR EXTRA TROPICAL STORM-INDIA
WESTERLIES
DIRECTION OF MOVEMENT OF WESTERIES
EASTWARD
ORGIN OF WESTERLIES
MEDITEERRANEAN
BLACK
CAPSIAN
WESTERLIES WEATHER
HIGH NIGHT TMEPERATURE
CLOUDY SKY UNUSUAL WIND
WESTERLIES
WESTELY CROPS
WHEAT,MUSTARD,GRAM
WEAK WESTERN DISTURBANCE
CROP FAILURE
HEAT CAPACITY OF OCEAN
HIGHER THAN LAND
CONTINENTAL EFFECT
T ON LAND CHANGES RAPIDLY
WILLY WILLY
AUSTRALIA
TYPHOON
CHINA SEA
TORANDOES
COASTAL US
HURRICANES
CARIBBEAN SEEA
TROPICAL CYLONES/
TYPHOONS/HURRICANES
SOUTH PACIFIC AND INDIAN OCEAN
TROPICAL CYCLONES
ATLANTIC OCEAN
EASTERN NORTH PACIFIC OCEAN
HURRICANES
WESTERN PACIFIC OCEAN AND NORTHERN INDIAN OCEAN
TYPHOONS
WARM OCEAN CURRENT IN
WESTERN PART OF OCEAN
EASTERN PART OF CONTIANENT
SUBTROPICAL HIGH PRESSURE AREAS TO EQUATORIAL LOW PRESSURE AREAS
TRADE WINDS
SUBTROPICAL HIGH PRESSURE BELT TO SUB POLAR LOW PRESSURE BELT
WESTERLIES
WESTELY DIRECTIONIN NH
SOUTH WEST TO NORTH EAST
WESTELY DIRECTIONIN SH
NORTH WEST TO SOUTH EAST
WESTERLIES STRONGER IN
SOUTHERN HEMISPHERE
WEESTERLIES WEAK IN NH DUE TO
MOUNTAIN BARRIERS
SATURATED
FULL CAPACITY MOISTURE AT GIVEN TEMP
RH =100%
DEW POINT
TEMPERATURE@SATURATION
DEWPOINT
DEW POINT RESULT
THIN LAYER OF AIR NEAR GROUND—-COLD ENOUGH TO CONDENSATE
DEW IS MOST LIKELY TO FORM
CALM CLEAR NIGHT—.STABILITY
CLOUDY NIGHT
HIGH TEMPERATURE
ATMOSPHERE REFLECTED WAVELENGTH
SHORT WAVES
MJO
MADDEN JULIAN OSCILLATION
MJO AFFECTS
INDIAN AND PACIFIC OCEAN
MJO DEFINED AS
INTRA SEASONAL TROPICAL CLIMATE VARIABLITY
EL NINO+MJO
DETRIMENTAL TO INDIAN CLIMATE
MEANDERING JET STREAMS
ROSSBY WAVES
JET STREAM FLOWS THROUGH
UPPER LAYERS OF TROPOSHERE
JET STREAM CAUSE
AIR MASSES OF DIFFERENT TEMP MEETS
WHAT DETERMINES ET STREAM
SURFACE TEMPERATURE
CIRCLE THE EARTH AS POLES AS CENTER
JET STREAM (CIRCUMPOLAR)
CM UH GBW-JET STREM
CIRCUMPOLAR
MEANDERING
UPPPER TROPOSHERIC’
HIGH VELOCITY
GEOSTROPIC STREAMS
BOUND BY LOW SPEED WINDS
WESTERLIES(UPPER)
CAUSE OF ROSSBY WAVES
VARIATION IN THE CORIALIS EFFECT
LOW T CONTRAST—->________________—–>MEANDERING
SLOW JET STREAM AND WEAK CORIALIS FORCE
JUNE 21
SUMMER SOLISTICE
PLANTS SOLAR USE
RESPIRATION(50%)—>STORAGE——>PHOTOSYNTHESIS(0.1%)
HIGH ALBEDO SUBSTANCE
SNOW
SEQUENCE OF ALBEDO
ICE>WATER>SOIL
WIND DIRECTION
WIND VANE
JET STREAMM BIFURCATION
TIBETIAN HIGHLAND
INDIAN JET STREAM
SOUTHERN ONE
SOUTH JET STREAM
WINTER WEATHER IN INDIA
WESTERLY PRESIPITATION HIGH
WEST AND NORTH
ELNINO
WARM CURRENT IN PERU
LOW PRESSURE ZONE IN EQUATOR
INTER TROPICAL CONERGENCE ZONE
ITCZ AIR
CONVERGE AND ASCEND
ITCZ IN 25DEG N
MONSOON TROUGH
MONSOON TROUGH
NW(THAR) TO PATNA
CHOTANAGPUR EAST-SOUTH EAST
BREAK OR BURST OF MONSOON
SUDDEN MOISTURE WIND+THUNDER+LIGHTNING
MANGO SHOWER
KERELA-KARNATAKA PREMONSOON
BLOSSOM SHOWERR
KERELA COFFEE
NOR WESTERS
KALBAISAKSHI
KALBAISAKSHI IN ASSAM
BARDOSILA
KALBAISAKSHI USE
TEA ,JUTE ,RICE(PRE MONSOON)
HOT DRY OPPRESSING WIND IN NORTHERN PLAIN
LOO
AMW-MONSOON WITH SHORT DRY SEASON
WEEST COAST OF INDIA SOUTH OF GOA
AS-MONSOON WITH DRY SUMMER
CORAMENDAL COAST TN
AW-TROPIICAL SAVANNAH
PENINSULAR PLATEAU
SOUTH OF TROPIC OF CANCER
BShw SEMI ARIAD STEPPE
GUJARAT
RAJATHAN
PUNJAB
BWhw-hot desert
extreme west rajasthan
Cwg-monsoon with dry winter
ganga plain
Dfc-cold humid winter with short summer
ARUNACHAL PRADESH
E-POLAR TYPE
JK
UTTARKHAND
HIMACHA PRADESH
LATE SUMMER
TROPICAL CYCLONES