What are the Different Types of Seaweeds, and How Do They

Download Report

Transcript What are the Different Types of Seaweeds, and How Do They

How Does Heat Transfer Affect Climate?
– The Horse Latitudes and The Intertropical Convergence Zone
• Dry air sinks at about 30⁰N and 30⁰S latitudes  locations of deserts; great
evaporation from ocean; often lack winds  “Horse Latitudes”
• The Intertropical Convergence Zone: ~ equator; trade winds converge, warm air
rises; often lack winds  “Doldrums”
– Ocean Currents Affect Regional Climates
• Example: San Francisco cooled by California Current, while Washington D.C.
warmed by Gulf Stream (both cities at same latitude)
– Monsoons and Cyclones
• Monsoons: seasonal wind patterns caused by heating and cooling of continents;
in summer, warm air rises over land, draws in moist warm air from ocean,
which rises and cools  heavy rainfall; common in India, Southeast Asia
• Cyclones: rotating storm systems around low-pressure center (eye of storm);
tropical cyclones (typhoons in Pacific, hurricanes in Atlantic) fueled by
warm water, draw in moist tropical air; extratropical cyclones form where
polar winds meet the westerlies (lead to unstable air, thunderstorms);
cyclones rotate counterclockwise in the Northern Hemisphere, clockwise in
the Southern Hemisphere
– Clouds and the Hydrologic Cycle
• The Water (Hydrologic) Cycle: includes evaporation, condensation, precipitation
• Clouds (condensed water vapor) trap heat but also reflect energy (white)
Figure 8-20
Figure 7-9
Figures 8-21 and 8-22
Figure 7-16
Figure 8-4
Figure 8-5
Is the Ozone Layer Still Threatened?
• Stratospheric Ozone Depletion
– Ozone a component of smog in lower atmosphere; in
upper atmosphere, shields Earth from UVB radiation
– Chlorofluorocarbons (CFC’s) lighter than air, rise to
upper atmosphere, where they stick to ice crystals;
each molecule able to destroy many ozone molecules
(most during summer); Antarctic ozone hole detected in
1985, Arctic ozone hole detected in early 1990’s; global
ozone declining (ex. Toronto, UV increased 5.3% per
year from 1989-1993)
– Effects of UV: skin cancers, stress immune systems,
coral bleaching, reduces productivity of phytoplankton
– International Response: Montreal Protocol (1987) phased
out production of CFC’s, but existing CFC’s stable
(long-lived; ex. freon)
Figure 8-2
Figure 8-3
What Evidence Supports the Theory of
Global Warming?
• A theory, supported by multiple lines of evidence (that
current observed warming trend is due largely to
human-caused influences)
– Greenhouse Effect: greenhouse gases trap warm air in lower
atmosphere (esp. carbon dioxide, methane, and carbon
monoxide)
– Combustion of fossil fuels adds CO2 to atmosphere; deforestation
is often via burning (combustion) and loss of trees reduces
uptake of carbon dioxide; more cattle  more methane
(proposal for effort to measure this effect laughed out of U.S.
Congress as “cow-fart study”)
– Observed: rise in atmospheric CO2; global atmospheric and
oceanic warming; rising sea levels (Tuvalu, Kiribati, other
Pacific islands flooding); retreat of mountain glaciers, Arctic ice
thinned, Antarctic ice shelves apparently breaking up;
tropical diseases and insects spreading; regional climates
shifting, affecting species ranges and causing extinctions;
widespread coral bleaching; lower heating costs on the
“bright side”
Figures 16-2 and 16-3
What are the Predicted Effects of Global
Warming and the International Response?
– Predicted: approx. 6°C rise by 2100; warming of tundra releases more
CO2, melting of polar ice reduces reflection of energy by white ice and
accelerates melting (vicious cycles); melting of West Antarctic ice sheet
would raise sea level by 20 feet, flooding London, New York, Florida,
New Orleans (among others); cooling of Northern Europe due to likely
disruption of Gulf Stream current by melting Arctic (more icebergs will
also endanger ships); rise in intensity of tropical cyclones due to
warmer water temperature
– Debate among specialists is mainly regarding the ocean’s role in the
absorption of CO2 (but note that levels steadily rising in atmosphere,
corresponding to steady rise in combustion/emissions)
– Public debate mainly regarding Earth’s natural cycles of warming/cooling
and lack of “definite proof”; also regarding economic costs of reducing
carbon emissions
– International Response: Rio Earth Summit (1992) – agreed that Global
Warming is serious problem and response needed by year 2000
(George Bush Sr. signed); Kyoto Accord (1998) – signed by nearly all
nations; Copenhagen (Dec. 2009); Adapt (?): sea walls planned in
Thailand and Bangladesh