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Lecture 7 S. American Lecture 7 S. American Climate Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation
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Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Jan 11, 2016

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Page 1: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Lecture 7 S. American ClimateLecture 7 S. American Climate

• Physical Settings

• Circulation controls

• Climate Change — Impacts of Amazonian Deforestation

Page 2: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Like Africa, primarily a tropical continent

Distinguish characteristic is the unbroken, high Andes Mt. chain that run the entire length near its west coast — allow the greatest meridional penetration of air masses anywhere in the S.H.

Continent extends farther poleward than any other S.H. continents — 56S, coming within 7 degree of Antarctic peninsula

Topography

fT

mT

mT

Mid

-latit

udin

al cy

clon

ic zo

ne

Page 3: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.
Page 4: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The Guiana current is fed by the North Brazil Current a major source of water for the Caribbean Sea. Water transported by the Guiana current also mixes with tropical waters from the N. Equatorial Current and eventually feeds the circulation of the N. Atlantic subtropical Gyre, via the Caribbean, Yucatan, Loop, and Florida currents.

Page 5: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The N. Brazil current transports a significant amount of water, including freshwater from the Amazon, northwestward along the coast of northern Brazil, French Guiana, and Suriname. It is fed by the S. Equatorial Current and part of it becomes the Guiana Current.

Page 6: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The Brazil current is the western boundary current of the South Atlantic subtropical gyre. Near 22 S, the Brazil current splits; one component flows eastward and the other component hugs the coast and flows toward the southwest and interacts with the colder Malvinas Current.

Northern boundary of SACZ

Page 7: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The Malvinas current is the northward flow component of the S. Atlantic subpolar gyre. It transports cold water along the coast of S. America and this water mixes with warmer waters of the Brazil current in an region known as the Brazil-Malvinas confluence.

Southern boundary of SACZ

Page 8: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The Peru Current (or Humboldt Current) is a cold ocean current that flows northward off the west coast of S.A. It becomes a major part of the westward South Equatorial Current. This current originates in the Southern Ocean near the Antarctic, and is thus about 7-8 C° cooler than the ocean at similar latitudes. The cold water cools down the air, creating the coastal deserts of Chile: the Atacama and Peru. However, the Humbolt Current brings nutrient-rich seawater into the region, forming the basis for a rich fishing industry on Peru and Chile.

Page 9: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

ANCHOVY SARDINE

JACK MACKERELPACIFIC MACKEREL

MAIN FISHERY RESOURCESMAIN FISHERY RESOURCES

DEMERSAL

DEMERSAL

INVERTEBRATES

INVERTEBRATES

HAKE

LIGHTFISH

PELAGICPELAGIC

PERUVIAN SCALLOP

JUMBO FLYING SQUID

Page 10: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Baron Alexander von Humboldt (September 14, 1769-May 6, 1859) was a Prussian naturalist and explorer who explored much of Central and South America. Humboldt and his friend, the French medical doctor/botanist Aime-Jacques-Alexandre Goujoud Bonpland (1773-1858), explored the coast of Venezuela, the Amazon and Orinoco Rivers, and much of Peru, Ecuador, Colombia and Mexico (1799-1805). On their many expeditions, Humboldt and Bonpland collected plant, animal, and mineral specimens, studied electricity (including discovering the first animal that produced electricity, Electrophorus electricus, the electric eel), did extensive mapping of northern South America, climbed mountains (and set altitude records), observed astronomical phenomena, and performed many scientific observations. The scientist Carlos Montufar (who later became a revolutionary in Ecuador) acconpanied them on part of the trip.

Humboldt discovered what is now called the Humboldt Current off the west coast of South America, while he was investigating why the interior of Peru was so dry. It is a cold ocean current that runs along much of the western coast of South America, and is also known as the Peru Current. Humboldt was the first European to witness native South Americans preparing curare arrow poison from a vine. He was also the first person to recognize the need to preserve the cinchona plant (its bark contains quinine, which is used to cure malaria, and it was terribly over-harvested at the time). Humboldt was the first person to make accurate drawings of Inca ruins in South America (he visited the ruins at Canar, Peru). Humboldt and Bonpland first discovered and mapped the Casiquiare Canal, the only natural canal in the world that connects two major rivers (the Orinoco River and the Negro River, a tributary of the Amazon). Humboldt was also the first person to discover the importance of guano (the dried droppings from fish-eating birds); it is an excellent fertilizer. After their South American expeditions, Humboldt and Bonpland visited the USA and were guests of President Thomas Jefferson in Washington, D.C., for three months in 1804 (their visit happened just after Jefferson had sent Lewis and Clark to explore the western US). At the age of 60, Humboldt traveled to the Ural mountains in Siberia and to Central Asia to study the weather. He wrote extensively of his travels and discoveries. One of his books, A Personal Narrative inspired a young Charles Darwin. His last work was his multi-volume book, Kosmos, which tried to unify all of science. Humboldt died at age 90 (leaving Kosmos unfinished), and is buried in Tegel, Germany. Many landmarks in the Americas, including a current, a river, a mountain range, a reservoir, a salt marsh, parks, many counties and towns are named for Humboldt. On the moon, the Mare Humboldtianum (Humboldt's Sea) was named for Humboldt.

Page 11: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

The cold currents around the Galapagos cause garua (mist) for part of the year. Early sailors thought the islands were enchanted as a result of their frequent disappearance.

Page 12: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

View of clouds over the ocean off Peru

Page 13: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Sunset over the southeastern Pacific from Paracas bay (14S, 76W), Peru.

Page 14: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Amazon rainforest, near Iquitos

Peru rainforest in eastern Peru

Page 15: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Altiplano plateau, Peru

Atacama desert, Chilean coast

Page 16: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Trewartha Climatic Classification System

Page 17: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

• Physical Settings

• Circulation controls

• Climate Change — Impacts of Amazonian Deforestation

Page 18: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Chaco Low

Page 19: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Positionally Stable Pacific Subtropical HighThe shape of the west coast of S.A. forms a near-perfect “basin” into which the S. Pacific STH can fit snugly and maintain contact with the continent almost to the equator

No other STH is so positionally stable and so perfectly anchored along a coast; produces maximum subsidence in the coastal area

Page 20: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Less “Unstable” Influences of Atlantic Subtropical High

To the east, air in the Cf region (Brazil) is not nearly as unstable as that in the Cf region of N. America (i.e. SE of U.S.) due to continent’s shape which bulges eastward into the influence of the more stable part of the South Atlantic STH.

Page 21: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Unique ITCZ

Behavior

Intrusion of Cold Front

Page 22: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.
Page 23: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

低層環流與降雨

Page 24: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.
Page 25: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Moisture sources of La Plata basin of southeastern S.A.

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Mean calendar date of onset of South American monsoon

Page 28: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.
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Page 34: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

• Physical Settings

• Circulation controls

• Climate Change — Impacts of Amazonian Deforestation

Page 35: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Title

Body text

Deforestation: Rondonia, BrazilDeforestation: Rondonia, Brazil

•1975 -Healthy natural vegetation

•1986 -“Fishbone” pattern on the landscape indicate agriculture fields

•2000 -Agriculture continues to replace forest cover.Satellite images reveal in startling detail

the signs of human impact on the landscape. Evidence that people have become a powerful force capable of reshaping the Earth’s environment is everywhere.

Page 36: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

雨林消失對氣候的衝擊

1.改變蒸發蒸散作用的速率

2.改變其在碳循環中扮演的源與匯角色

3.改變區域水循環

逕流增加或減少 ?

Page 37: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

亞馬遜河流域的熱帶森林區,每年約有100~ 200萬公頃的森林被清除,多項研究已顯示,如此高速率、大規模砍燒森林會增加大氣中 CO2 濃度,改變當地的水文及氣候。衛星照片顯示,東部與南部是消退最快速的地區, 1978年森林消退的面積是 78000km2 ,1988年達到230000km2 。 沒有控制與有控制的森林採伐所造成的

a. 地表溫度 (C); b. 深土溫度(C);c. 總降水量 (mm);d. 蒸發量(mm)等的變化 ◦

Page 38: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Differences between simulated parameters:

Short grass minus Forest

Decrease in precipitation

Increase in precipitation

Local temperature increase reaching until 5°C

Page 39: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Differences between simulated parameters:

Short grass minus Forest

The increase in maximum temperature is larger than the increase in minimum temperature

Page 40: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Foliage TemperatureGround Temperature

Ground and foliage temperature is higher in the short grass in the Amazon region, and is lower in other areas

Differences between simulated parameters:

Short grass minus Forest

Page 41: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Differences between simulated parameters: Differences between simulated parameters: Short grass minus ForestShort grass minus Forest

Dryer

Moister

Page 42: Lecture 7 S. American Climate Physical Settings Circulation controls Climate Change — Impacts of Amazonian Deforestation.

Differences between simulated parameters: Differences between simulated parameters: Short grass minus ForestShort grass minus Forest

Over the Amazon the lower level winds ( σ=1) became more intense in the short grass