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MIDDLE-EAST Haiman, Oman (20°N) www.esrl.noaa.gov/psd/cgi-bin/data/composites/printpage.pl Figure 5.14 and 7.6

MIDDLE-EAST Haiman, Oman (20°N) Figure 5.14 and 7.6

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Page 1: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MIDDLE-EAST

Haiman, Oman (20°N)

http://www.esrl.noaa.gov/psd/cgi-bin/data/composites/printpage.pl

Figure 5.14 and 7.6

Page 2: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6
Page 3: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MADAGASCAR

Toamasina (18°S)

Page 4: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MADAGASCAR

Toliara (23°S)

Page 5: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MARITIME CONTINENT-MALAYSIA

Kuala Lumpur (3°N)

RH for other months?

Page 6: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MIDLATITUDE CLIMATES

1. Dry subtropical 2. Moist subtropical3. Mediterranean4. Marine west-coast5. Dry midlatitude6. Moist continental

DRY SUBTROPICAL

• Low precipitation, great annual temperature range

•In: North and South Africa, Patagonia (South America), Southern Australia, North America (NW Mexico, SW US)

•Factor: subtropical highs

Patagonia, Argentina

Page 7: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MOIST SUBTROPICAL

•Abundant rainfall in summer and winter on eastern side of continents (more in summer)

•In: South America (limit Argentina, Uruguay and brazil), Southern China, Australia, SE of US

• Factors: •In summer: flow of warm and moist air onto eastern side of continents (mT air mass). •In winter: wave cyclones

Montevideo, Uruguay

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Page 8: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MEDITERRANEAN

• Wet winter and very dry summer (different from other climate types)•Factors: pole-ward movement of high pressure cells (Fig 5.14)during summer. Dry cT air mass dominates

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Athens, Greece

Page 9: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

MARINE WEST-COAST

•Precipitation all months with maximum in winter•Small annual temperature range• Westerlies from ocean, mP air masses. When coast is mountainous: orographic effect•Summer: subtropical high pressure poleward less rainfall

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Bordeaux, France

Page 10: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

DRY MIDLATITUDE•Very low precipitation•In: interior regions of North America and Eurasia•Factors: rain shadow of mountains, mP air mass is blocked cP dominates•Summer: convection rainfall

MOIST CONTINENTAL

•Precipitation all year, increases in summer. Strong annual cycle of temperature.•In: North America and Eurasia

•Factors: Polar front zone (mT ,cP, mP air masses interaction)•Summer: invade of mT•Winter: cP and cA air masses

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Krakow, Poland

Gobi Desert

Page 11: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

HIGH LATITUDE CLIMATES

1. Boreal Forest2. Tundra3. Ice Sheet

BOREAL FOREST

• Long winters and short summers. Greatest annual range of temperature. Precipitation increases in summer but is generally low

• Regions with cP air mass and invasion of cA air mass• Summer: traveling wave cyclones

Page 12: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6

TUNDRA

• Long and severe winters. Short mild season

• cP, mP and cA air masses. Influence of ocean moderates cold temperatures in coast regions

ICE SHEET

• Lowest temperatures, no above 0°C• Greenland, Antartica, polar sea ice of Arctic Ocean• cA and cAA air masses

Vostok (78°S): Russian base in Antartica. One of if not the coldest place on Earth. Mean Temp: -67.0 F or –55.0°C

Page 13: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6
Page 14: MIDDLE-EAST Haiman, Oman (20°N)  Figure 5.14 and 7.6