CLIMATOLOGY And It's APPLICATION - RTC, Regional Training ...

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Instead, there are semi-permanent high- and low-pressure systems. They are semipermanent because they vary in strength or position throughout the year. Wintertime ; Polar highs develop over Siberia and Canada The Pacific High, Azores High (parts of the subtropical high pressure system) Aleutian Low and Icelandic Low form Summertime ; The Azores high migrates westward and intensifies to become the Bermuda High The Pacific high also moves westward and intensifies Polar highs are replaced by low pressure A low pressure region forms over southern Asia
The Monthly Average Temperature The Monthly Average Precipitation Winter Summer Year Annual Range NH 8.1C 22.4C 15.2C 14.3C SH 9.7C 17.0C 13.3C 7.3C Differe nce -1.6C 5.4C 1.9C 7.0C
Page 1 and 2: CLIMATOLOGY And It’s APPLICATION
Page 3 and 4: Climate is defined as the collectiv
Page 5 and 6: Aim’s of climatology, is the obje
Page 7 and 8: CLIMATOLOGICAL DIVISION Spatial Sca
Page 9 and 10: As with the different scales of wea
Page 11 and 12: Paleoclimatology Determining past c
Page 13 and 14: The five basic climate controls are
Page 15 and 16: Atmospheric Circulation One way to
Page 17 and 18: 1. Tropical cell (Hadley cell) - Lo
Page 19 and 20: Pressure belts: The three-cell circ
Page 21: Global climate is the largest spati
Page 25 and 26: Large mountains influence regional
Page 27 and 28: World vegetation
Page 29 and 30: However, climate observations diffe
Page 31 and 32: 3. The details and history of local
Page 33 and 34: 6. Operation of historically‐unin
Page 35 and 36: 9. The conversion of research obser
Page 37: “PEACE AT HOME, PEACE IN THE WORL

CLIMATOLOGY And It's APPLICATION - RTC, Regional Training ...

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