CYCLONES
K.SUGUNA.R
PGT GEO
WINDS
• HORIZONTAL MOVEMENT– WIND
• VERTICAL MOVEMENT ---- AIR CURRENT
TYPES OF WINDS
• PLANETARY WINDS
• SEASONAL WINDS
• LOCAL WINDS
PLANETARY WINDS• TRADE WINDS
• ANTI TRADE WINDS
• POLAR WINDS
SEASONAL WINDS
• MONSOON WINDS-
• NORTH EAST MONSOON
• SOUTHWEST MONSOON
LOCAL WINDS
• LAND BREEZE AND SEA BREEZE
• MOUNTAIN AND VALLEY BREEZE
• CHINOOK WINDS
• LOO WINDS
CYCLONES
• LOW PRESSURE DEPRESSIONS
• STRONG WINDS
• CYCLONIC STORMS
DIFFERENT NAMES OF CYCLONES
• COMMON NAME : TROPICAL CYCLONE
• INDIAN OCEAN :CYCLONES
• ATLANTIC OCEAN :HURRICANES
• WESTERN PACIFIC
(JAPAN &CHINA SEA) :TYPHOONS
WESTERN AUSTRALIA: WILLY WILLIES
CONDITIONS FAVOURABLE FOR THE FORMATION
• LARGE SEA SURFACE WITH TEMPERATURE ABOVE 270 C
• PRESENCE OF CORIOLIS FORCE• SMALL VARIATION IN THE VERTICAL WIND SPEED• A PRE-EXISTING WEAK LOW PRESSURE AREA• DIVERGENCE OF AIR IN THE UPPER LAYER
FORMATION OF CYCLONES
• EYE OF THE CYCLONE – CENTRE OF THE CYCLONE
• EYE WALL – RISING AIR • CUMULONIMBUS CLOUDS
TROPICAL CYCLONES• OCCUR IN TROPICAL REGIONS• STRONG AND POWERFUL• OCCUR IN SEA ONLY• ON LAND- IT DISSIPATES
TEMPERATE CYCLONES
• CAUSED IN MIDDLE AND HIGH LATITUDES• CAUSED IN FRONTAL ZONES• OCCUR IN BOTH LAND AND SEA• COVER A LARGER AREA
ANTICYCLONES• HIGH PRESSURE ZONES
• WINDS-BLOW OUTWARDS
• NO RAINFALL
THUNDER STORMS • CAUSED BY INTENSE CONVECTION ON MOIST HOT DAYS• IS A WELL GROWN CUMULONIMBUS CLOUDS PRODUCING
THUNDER AND LIGHTENING.• SOMETIMES CAUSES HAILSTROMS• IF THERE IS INSUFFICIENT MOISTURE –DUST STORMS
TORNADOES• FROM SEVERE THUNDERSTORMS SOMETIMES SPIRALLING WIND
DESCENDSLIKE A TRUNK OF ELEPHANT WITH GREAT FORCE.• CAUSES MASSIVE DESTRUCTION ON ITS WAY.• COMMON IN MIDDLE LATITUDES• THE TORNADO OVER THE SEA• IS CALLED WATER SPROUTS