Relation Between Global Warming And Tropical Storm

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    Relation Between Global Warming And Tropical Storm - Presentation Transcript

    1.  
      • Thunderstorm categorized by cyclonic wind activity developed in Low Pressure region of Tropics.
      • Wind speed belonging to 63-112 km/h.
      • Controls the Global Atmospheric Circulation Mechanism in Troposphere
      • Ex. Hurricane,Typhon,Katrina,Rita, Includes tropical depressions, tropical storms
      • Tropical Cyclone occur when Sea Surface Temperature ( SST )>26 0 C
      • TROPICS
      • Located 23½° N to 23½° S.
      • Large amount of solar radiation.
      • Little seasonal variation.
      • Warm water is the source of tremendous
      • latent heat source.
      • High relative humidity promotes cumulus cloud development.
      • Surface winds from the east
      TROPICS
      • Sun generated tremendous heat increase the percentage of Moisture in air of Sea.
      • Higher wind speed and create a Low Pressure zone .
      • More Condensation of moisture in air.
      • Enthalpy of condensed moisture generate power in Warm core .
      • Convective available Potential Energy is effected by large scale subsiding air.
      • Starting of Cyclonic wind rotation depending upon the rotation of earth.
      • # Anticlockwise rotation in Northern Hemisphere.
      • # Clockwise rotation in southern Hemisphere.
      • fig :1
      • Pressure gradiant force is represented by Blue Arrows.
      • Coriolis force is repreasented by Red Arrows.
      • Huge amount of greenhouse gas create a cover over the atmosphere.
      • Sun generated heat can’t reflect to space.
      • Hotter atmosphere, higher SST.
      • Last 35 yr ,Global SST jump .5 0 C
      • Fig2: Global Mean Surface temp. Anomalies Fig3: Sea Surface Temp Anomalies
      • Atmospheric water vapour pressure increases ,specially at tropical regain by increasing SST.
      • water vapour increase 1.3% per decades.
      • Surface pressure falls
      • Enhancing tropical convection
      • More power generate by huge enthalpy of condensed moisture.
      • Tropical storm intensity and frequency increase.
      • Fig4:
      • The Low Pressure zone
      • occurs at higher SST
      • Due to SST increase, wind speed also change in upward dip in fig 5 and cyclone intensity increase.
      • Fig5:Atlantic Tropical
      • Cyclone intensity vs SST
      • Fig 6: Global Hurricane intensity change Fig 7:Regional hurricane intensity change
    2. YEAR AVG. STORM AVG. HURRICANE AVG.DEVASTATIVE HURRICANE 1970-2004 8.6 5 1.5 1995-2004 13.6 7.8 8.6
    3.  
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