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Seasonal Shift of the ICTZ

Seasonal Shift of the ICTZ. Applied to West Africa. SUN OVERHEAD 23 ½ºS. POSITION OF THE THREE CELLS IN DECEMBER. Polar Cell. The sun is overhead at the Tropic of Capricorn, 23 ºS of the Equator. Ferrel Cell. Hadley Cell.

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Seasonal Shift of the ICTZ

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  1. Seasonal Shift of the ICTZ Applied to West Africa

  2. SUN OVERHEAD 23½ºS POSITION OF THE THREE CELLS IN DECEMBER Polar Cell The sun is overhead at the Tropic of Capricorn, 23ºS of the Equator. Ferrel Cell Hadley Cell The cells shift southwards as the heat equator is in the southern hemisphere. Hadley Cell Ferrel Cell Q Polar Cell

  3. SUN OVERHEAD 23½ºN POSITION OF THE THREE CELLS IN JUNE Polar Cell The sun is overhead at the Tropic of Cancer, 23ºN of the Equator. Ferrel Cell Hadley Cell Hadley Cell The cells shift northwards as the heat equator is in the northern hemisphere. Ferrel Cell Polar Cell Q

  4. Sub-tropical high pressure Equatorial low pressure Sub-tropical high pressure Inter-Tropical Convergence Zone THE INTER-TROPICAL CONVERGENCE ZONE IN THE NORTHERN HEMISPHERE: The winds that blow to the equatorial low pressure belt are called the North East Trade Winds IN THE SOUTHERN HEMISPHERE: The winds that blow to the equatorial low pressure belt are called the South East Trade Winds The line along which they converge (meet) is called the INTER-TROPICAL CONVERGENCE ZONE. This is often abbreviated to ITCZ Q

  5. Sub-tropical high pressure Equatorial low pressure Sub-tropical high pressure Inter-Tropical Convergence Zone THE INTER-TROPICAL CONVERGENCE ZONE IN THE NORTHERN HEMISPHERE OVER WEST AFRICA The sub-tropical high pressure belt develops over the Sahara so is hot and dry. This is known as continental Tropical (cT) air. IN THE SOUTHERN HEMISPHERE OVER WEST AFRICA The sub-tropical high pressure belt develops over the Atlantic so is warm and moist. This is known at maritime Tropical (mT) air. Q

  6. Sub-tropical high pressure SOLAR ENERGY Equatorial low pressure Inter-Tropical Convergence Zone Sub-tropical high pressure THE ITCZ IN DECEMBER In December, the zone of maximum insolation (solar energy) is south of the Equator. This means that the wind belts shift southwards. This means that winds blow out of the sub-tropical high pressure area over the Sahara, and take dry air from the continental Tropical (cT) air mass across most of West Africa. This causes a dry season. Moist air from the maritimeTropical (mT) air mass from the Atlantic cannot reach far inland, where there is a dry season. Q

  7. Sub-tropical high pressure SOLAR ENERGY Equatorial low pressure Inter-Tropical Convergence Zone Sub-tropical high pressure THE ITCZ IN JUNE By contrast, in June, the zone of maximum insolation is well to the north of the Equator. This means that the wind belts shift northwards. Moist maritime Tropical air from the Atlantic now reaches far inland, where there is a rainy season. These winds flow northwards to the ITCZ to replace air that has become unstable and risen. The winds blow out of the sub-tropical high pressure area over the Sahara, now only affect the northern part of sub-Saharan Africa.

  8. The ITCZ in West Africa

  9. THE EFFECT OF THE SUN’S MIGRATION ON SEASONAL TEMPERATURES AFRICA TROPIC OF CANCER 23½ºN TROPIC OF CANCER 23½ºN EQUATOR 0º EQUATOR 0º TROPIC OF CAPRICORN 23½ºS TROPIC OF CAPRICORN 23½ºS AFRICA – TEMPERATURES IN JANUARY AFRICA – TEMPERATURES IN JULY Because the sun is overhead in the southern hemisphere, it is the south that is hottest, (shown by the red areas). The Sahara stands out as a cooler, (lighter coloured), area. In July, with the sun overhead north of the Equator, the Sahara is clearly much hotter than the rest of the continent.

  10. POSITION OF THE ITCZ IN DECEMBER ITCZ ITCZ Click here to find out about stable air Clickhere to find out about unstable air In December the sun is overhead in the southern hemisphere. The ITCZ is found to the south, where there is maximum insolation. The sea stays a fairly constant temperature, so the ITCZ runs just along the coast in WAfrica. Sub-tropical high pressure NE Trade Winds – locally called the Harmattan.They are stable and dry as they originate from over the Sahara Desert. Only the coastal fringe receives rain from the unstable mT air at this time of year Further north, the area is under the influence of the Harmattan, (stable, dry cT air blowing out of the Saharan high pressure area). SE Trade Winds They are unstable and moist as they originate from over the Atlantic Ocean. EQUATOR 0º

  11. MIGRATION OF THE ITCZ FROM DEC. TO JUNE Between December and June, progress through the Earth’s orbit causes the sun to migrate northwards. Sub-tropical high pressure NE Trade Winds – locally called the Harmattan.They are stable and dry as they originate from over the Sahara Desert. As it does so, the ITCZ also moves further north, allowing moist mT air to reach progressively further inland, brining the rainy season to West Africa. SE Trade Winds They are unstable and moist as they originate from over the Atlantic Ocean. EQUATOR 0º

  12. MIGRATION OF THE ITCZ FROM JUNE TO DEC. By late June, the sun begins to migrate southwards, and so does the ITCZ, following the zone of maximum insolation. Sub-tropical high pressure As the ITCZ moves further south, the Harmattan carries dry, stable cT air further south, bringing the dry season across more and more of West Africa. NE Trade Winds – locally called the Harmattan.They are stable and dry as they originate from over the Sahara Desert. SE Trade Winds They are unstable and moist as they originate from over the Atlantic Ocean. EQUATOR 0º

  13. Stable, dry, cT air from the Sahara moves southwards. It causes the dry season across this area THE ITCZ AND PRECIPITATION IN WINTER North South mT air right at the ITCZ is prevented from rising by stable cT air ITCZ Warm land surface makes the mT air unstable. It rises and rain falls a short way behind the ITCZ GULF OF GUINEA 20ºN 15ºN 10ºN 5ºN Based on a diagram from “Core Themes in Geography”, by Broadley & Cunningham

  14. Stable, dry, cT air from the Sahara moves southwards. It causes the dry season across this area THE ITCZ AND PRECIPITATION IN SUMMER South North Occasional rainfall Heaviest rainfall ITCZ Moist unstable mT air now reaches far inland, bringing rain to about 17ºN GULF OF GUINEA 20ºN 15ºN 10ºN 5ºN Based on a diagram from “Core Themes in Geography”, by Broadley & Cunningham

  15. Strong high pressure over Sahara causes strong subsidence. This prevents advance of ITCZ to northernmost areas. THE ITCZ AND PRECIPITATION IN A SUMMER DROUGHT North South Heaviest rainfall Occasional rainfall ITCZ Moist unstable mT air is prevented from reaching far inland. GULF OF GUINEA 20ºN 15ºN 10ºN 5ºN Based on a diagram from “Core Themes in Geography”, by Broadley & Cunningham

  16. RAINFALL IN WEST AFRICA 20ºN 3 250 15ºN 15 500 25 250 1000 36 60 500 2000 10ºN 110 3000 75 1000 3000 123 111 1000 5º 2000 2000 3000 3000 2000 KEY 3000 250 EQUATOR 0º Isohyet, with rainfall in mm Average number of days with rain 75

  17. With thanks to the source: http://www.ltscotland.org.uk/Images/globalcirculation_tcm4-123440.ppt by Nevis Hume and John Smith

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