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The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012
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The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

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Page 1: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

The Amazon BasinCE 397 Transboundary Waters

Christine Lynch

Feb 7, 2012

Page 2: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

The Amazon’s International Importance

Global Importance to:Water

Carbon Cycle

Climate

Biodiversity

Page 3: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Amazon Overview

The Amazon Basin is the largest basin on the planet, at over 6,100,000 km2

Its drainage area covers over 1/3 of the South American continent

The Amazon discharge (~220,800 m3/s) contributes over 20% of the total discharge of all global rivers

The amazon transports between 600 million and 1.2 billion tons of sediments per year

The Amazon is estimated to be between 6400 and 7100 km long from its headwaters in the Andes to its discharge in the Atlantic (second in length only to the Nile)

The Amazon affects the color and salinity of the Atlantic for nearly 200 miles from its delta

Page 4: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Amazon Overview

The Amazon has over 200 tributaries, 15 of which are over 1000 km in length, and 3 of which are over 3000 km in length

Over 1/3 of the total discharge is contributed by the Madiera and Negro rivers

The Amazon Rainforest, which is not confined to the Amazon river basin, is the most extensive and preserved rainforest in the world Makes up 60% of remaining tropical rainforests

Makes up 56% of remaining broad leaf forests

83% of the forest is still intact

Produces ~20% of the Earth’s oxygen Key component of the global carbon cycle

Page 5: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Division of the Amazon

The Amazon Basin is shared between 7 countries: Brazil

Peru

Ecuador

Bolivia

Columbia

Venezuela

Guyana

Languages include Portuguese, Spanish, and hundreds of critically endangered native languages

The Amazon Rainforest extends beyond the river basin boundaries and includes Suriname and French Guiana

Page 6: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Division of the Amazon

10.7

11.4

69.1

25.9

0.8 <0.1

Amazon Basin Countries by Area (%)

BoliviaPeruBrazil EcuadorColombia Venezuela Guyana

Page 7: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Division of the Amazon

Bolivia

Peru

Brazil

Ecuador

Colombia

Venezuela

Guyana

0 10 20 30 40 50 60 70

Country Area included in the Amazon Basin (%)

Page 8: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Division of the Amazon

Amazon Subbasins by Area

20%

11%

10%

7%7%

5%

5%

5%

4%

3%

2%

2%

2%2%

13%

1%

Amazon Subbasins by Area

Madeira Tocantins NegroXingu Tapajós PurusMarañónUcayali Caquetá-Japurá JuruáPutumayo-IçáTrombetas NapoUatumã OrinocoOther

Page 9: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Division of the Amazon Human density in the Amazon is low and concentrated in

urban areas 5 cities have >1,000,000 inhabitants, 3 cities have over 300,000

inhabitants. Major population centers are generally located along larger rivers

Deforested cities are “heat islands,” subject to flooding and having cloud to ground lighting occurring at rates >3 times as often as in nearby forests

The Brazilian Amazon, the most densely populated portion of the Amazon, has about 3.3 inhabitants/km2, much lower than the average of 20 inhabitants/km2 in the remainder of Brazil. The low population density is a preserving factor in the basin,

but results in a failure to prioritize collection of data

Though the population of the Amazon (~10 million) is less dense than that of the countries it is part of, its growth rates range from 5.2-7.2%, well above the national averages of Amazon countries

Page 10: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate

The Amazon Rainforest is a major climate regulator Absorbs incoming radiation at equator to lower

temperatures

Annual mean temperature over entire basin varies from 24 to 26˚C

Absorbs and stores moisture

Recycles between 1/2 and 2/3 of regional rainfall

Mean annual rainfall greatly varies spatially, generally oscillating between 1000-3600 mm with more at the mouth and less in the interior, but exceeding 8000 mm in the Andean coastal region

75% of the energy that drives atmospheric circulation comes from the heat released during tropical rainfall

Page 11: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate

The rainy season starts in the south in December, and gradually moves north through May. During this time the rains swell the rivers of Amazonia, creating extensive wetlands. (Images by Robert Simmon, based on data from the Global Precipitation Climatology Project)

Page 12: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate

El Niño Higher than normal temperatures in the Equatorial Pacific

Significantly reduces Amazon precipitation

Droughts

Fish are concentrated in deeper channels, making fishing easier and resulting in a decline in fish stock during subsequent years

La Niña Higher than normal temperatures in the Equatorial Pacific

Opposite effect – increased rainfall

Flooding

Page 13: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate - Deforestation Between 2000 and 2007, the Brazilian Amazon was

deforested at a rate of 19,368 km2/yr. During this time, an area of forest larger than Greece was destroyed Brazil is the world’s 4th largest climate polluter, with 75% of

their greenhouse gas emissions attributed to deforestation and land use change. 59% of this is from loss of forest and burning in the Amazon.

The removal of forest (done using slash and burn techniques) reduces the retention of humidity in the soil’s top layer for 1

meter in depth

Facilitates sudden evaporation of water previously retained in forest canopy

Increases albedo (reflectiveness) and temperature

Reduces porosity of soil, causing faster rainfall drainage, erosion, and silting of rivers and lakes

Page 14: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate - Deforestation Widespread convection has been documented in

deforested areas, forming shallow cumulous clouds which usually do not evolve into nimbus clouds and as a result may not produce rain

Forests expel hygroscopic salts and organic fibers along with water during evapotranspiration, and these act as water vapor condensation nuclei at higher elevations. This process results in formation of abundant clouds and represents almost 50% of recycled rainfall.

The Amazon is estimated to store between 80-120 billion tons of carbon. If destroyed, it will emit roughly 50 times the annual greenhouse gas emissions from the U.S.

Amazon rain is generally acidic. It is unknown at this time whether this is due to naturally occurring carbonic acids, or nitrous and sulfuric acids from fossil fuel burning and deforestation

Page 15: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Climate - Deforestation Compared to the pasture it is generally replaced with:

Forests absorb ~11% more solar radiation

The average albedo of the Amazon forest is 13.4%, of pastures, 18%

The average temperature in the Amazon is ~ 24.1˚C, in pastures it is 33 ˚C

The daily temperature variation of Amazon soils at 20 cm did not exceed 2.8 ˚C, though under pastures it was 8 ˚C

The volumetric moisture content in the upper 1 m of pasture soil is about 15% less than under nearby forest

Deeper forest roots can pump more soil moisture to the surface, producing 20-30% more air humidity and consequently 5-20% more precipitation than pastures

Several numeric models have suggested that large-scale deforestation would diminish superficial drainage by 10-20% and increase the surface air temperature by 0.6-2 ˚C, resulting in huge changes in the regional water cycle

Page 16: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use

Land use tied to deforestation and thus inextricably connected to climate and water cycle

Early settlement of the Amazon occurred mainly in the várzeas due to their river resources, including the fertile alluvial soils which supported agriculture and cattle. These activities were supplemented by hunting and gathering. Hunting for subsistence and skins has virtually eliminated

turtles and freshwater manatees from some areas

Prior to 1960s, economy based on extraction of natural resources, primarily rubber, cocoa, and fish Rubber the main export until the beginning of the 20th century, when

competition from SE Asia, a decline in rubber demand, and fungal plague brought the decline of the Amazon’s rubber production around 1950

Page 17: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use Construction of roads and highways in the 1960s altered

social structure and settlement of the Amazon region Highways parallel to large rivers led to increased deforestation

along rivers

Logging companies built roads deep into forests and away from rivers, enabling extraction and export of timber but also of settlement away from rivers

Timber is collected primarily for export. Deforestation of flooded forests for timber (and cattle) remove important feeding grounds for several commercially valuable fish, and also negatively affects the harvesting of Brazilian Nuts

Road construction negatively impacted surface water by preventing normal flow, flooding some areas while drying others

Connected Amazon to the rest of Brazil

Allowed easier access to mining centers - after 60s mining of bauxite and gold became important and people began to migrate from the rivers to areas near these industries

Page 18: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use Mining

15% of the world’s supply of bauxite

Some of the largest suppliers of iron and steel to world markets

Mining is scattered but has environmental impacts – primarily alluvial gold

Gold mining contributes to high mercury levels in fish and releases geologic arsenic

Mining of bauxite in Oriximiná, Pará, almost destroyed Batata Lake by extensive silting, though there was no legal punishment for the company responsible

Agriculture Rice, cassava, corn, and beans are subsistence farmed, while

Soya, coffee, and cacao are produced commercially

Fertilizers create local eutrophication

Brazilian Nuts, rubber, and açaí, although many medicinal and aromatic plants are harvested for pharmaceutical and cosmetic industries

Page 19: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use - Cattle Cattle ranching is responsible for the majority of Amazon

deforestation

Brazil has the largest commercial cattle heard in the world and has been the world’s largest beef exporter since 2003

In 2006 cattle occupied 79.5% of land already in use in the Brazilian Legal Amazon (this includes forest outside of the Amazon Basin) and 3 head of cattle per inhabitant

Around 40% of Brazil’s cattle are located within the Amazon, and this is where the most growth or cattle ranching occurs

Belched methane from livestock constitutes roughly 30% of greenhouse gas emissions from agriculture, making it one of the largest agricultural sources.

Greenhouse gas emissions from beef are 13 kg CO2-eq per kg. This means consuming a kg of beef represents roughly the same greenhouse gas emissions as flying 100 km of a flight, per passenger.

Page 20: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use - Cattle

Page 21: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Land Use - CattleRates of deforestation are affected by international commodity price fluctuations, especially meat and soya. When the price of both products drop, deforestation rates decrease the following year.

Page 22: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Water Use Navigation

Ports in Iquitos (Peru) and Porto Velho city (Brazil) receive ships that travel over 3500 km along the rivers

Estimated that over 40,000 km of waterways within the basin are navigated by various types of craft

Not all rivers are navigable

Fishing Over 200 species of fish are exploited, but the commercial

market is based only on a few dozen

Of these two are already considered overexploited

Conflicts between local subsistence fishers and commercial fishermen in the várzea and industrial fishermen in the estuary

Protect healthy stocks from commercial practices

Introduction of alien species in Andean waters

Page 23: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Water Use - Dams

Hydroelectric energy is complemented by fuel-burning thermo-electric centers

Dams create habitat fragmentation, interrupt fish migration, and substitute river habitats with lake habitats Local extinction of migratory species possible but

unrecorded

Poor knowledge of species makes assessment of impacts difficult

Case study: Tucuruí Hydroelectric Dam on the Tocantins River

Page 24: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Water Use - Dams

47%

39%

6%

6%

1%

Dam Capacity (MW) by country

Brazil - 11 damsVenezuela - 1 damEcuador - 5 damsPeru - 7 damsBolivia - 4 dams

Page 25: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Water Use - Dams

Decomposition of submerged organic material creates greenhouse gases, including methane, which is released when pressure suddenly drops as water is released by the turbines

Page 26: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Water Use - Dams

According to Brazil’s National Institute for Space Research (INPE), the world’s 52,000 large dams contribute to more than 4% of the total warming impact of human activities, and dam reservoirs are the largest single source of human-caused methane emissions.

A molecule of methane does 34 times more damage than a molecule of CO2

According to one analysis, greenhouse emissions from hydroelectric production of the Curuá-Una Dam in Para, Brazil, were 3.5 times higher than if the electricity had been produced by its fossil fuel burning counterparts

Drying conditions in the Amazon may make hydropower a less viable power source

Page 27: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Health

Health is negatively impacted mostly in deforested areas Malaria, hepatitis, yellow fever, and dengue exhibit a

tendency to break out after habitats are modified

Arsenic has been found in rivers due to deforestation and mining (as well as a small amount of natural geologic arsenic from the Andes)

Mercury from gold mining has impacted fish In one village, the hair from people who ate fish contained

twice as much mercury as from those who didn’t

This was a village that obtained most of its protein from beef

Page 28: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Obligation of the Amazon Countries?

In 1990, the Brazilian Amazon contributed 3.5% of GDP, despite occupying over 45% of Brazil

“…rainforest land converted to cattle operations yields the landowner $60 per acre; if timber is harvested, the land is worth $400 per acre. However, if medicinal plants, fruits, nuts, rubber, chocolate, and other renewable and sustainable resources are harvested, the land will yield the landowner $2,400 per acre.” The Healing Power of Rainforest Herbs (Square One Publishers, Inc. Garden City, NY 11040, © Copyrighted 2004) By Leslie Taylor

Do you believe it is truly possible for countries to sustainably harvest from the Amazon in a way that is no less profitable than alternative methods?

If not, do you think is it the responsibility of the Amazon countries to sacrifice their economic potential for the good of the rainforest?

Page 29: The Amazon Basin CE 397 Transboundary Waters Christine Lynch Feb 7, 2012.

Questions?