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Climate is weather over time |
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Principle components of Earth's Climate system |
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insolation temperature air pressure air masses precipitation |
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polar ice sheet tundra taiga (cool summer) cold desert, cold steppe, humid continental mild summer mild altitude arid hot desert, midaltitutde semiarid and steppe, humid continental warm hot summer hot steppe, mediterranean dry summer subtropics, humid subtropics Tropical arid, tropical semi arid, seasonal wet and dry tropics savana, monsoon tropics, equatorial tropics rain forest |
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Rain forest Monsoon Savanna |
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– Climate is constantly moist and warm – Rainy all year – Convectional thunderstorms triggered by local heating and trade wind convergence |
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– Principally along coastal areas – Rainfall from 6-12 months of the year brought by the ITCZ – Dry season lasts one or more months |
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– ITCZ dominates during summers with wetter conditions – Dry conditions when ITCZ shifts away and high pressure dominates |
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plants adapted to seasonally dry water budgets |
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Humid subtropical: Marine west coast: Mediterranean: |
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– Hot summers, mild winters – Maritime tropical air masses produce convectional showers over land during summer – Frontal activity with polar air masses in winter |
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– Warm to cool summers, mild winters – Affected throughout the year by weather systems formed along polar front |
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– Dry summers, mild winters – Large-scale agriculture requires irrigation |
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Humid continental Subarctic: |
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– Hot to warm summers, cold winters – Maritime tropical air masses influence both humid continental moist-all-year and winter-dry climates – In North America, conflict between maritime tropical and continental polar in winter |
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– Cool summers to very cold winters – Boreal forests (fir, spruce, etc.) thin out to the north to the more open woodlands and tundra – Soils thin in areas once scoured by glaciers |
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Tundra: Ice caps and ice sheets Polar marine |
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– High latitude or high elevation – Land under continuous snow cover 8-10 months – Never warms above 10 oC – Small plants appear in spring |
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– Perpetually frozen – All months below freezing |
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– More moderate than polar continental – No month averages below -7 oC |
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Arid deserts: Semiarid steppes (flat grassland) |
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– Tropical, subtropical hot – Midlatitude cold |
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Semiarid steppes (flat grassland) |
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– Tropical, subtropical hot – Midlatitude cold occurs poleward of 30o latitude |
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Causes of recent global warming |
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– Release of greenhouse gases into the atmosphere due to burning of fossils fuels? – Recent temperature rise is just part of the natural cycle? |
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Intergovernmental Panel on Climate Change (IPCC) was created in |
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1988 to coordinate global climate-change research, climate forecasts, and formulation of policies |
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Carbon dioxide (CO2), methane (CH4) and water vapor are essential |
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warmers of the planet: – Without them the Earth would be an ice ball, 35o C colder |
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Sun’s energy enters the Earth’s atmosphere at relatively short wavelengths (mostly within visible range) |
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Process of the greenhouse effect |
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1. much of the incoming short wavelength, solar radiation, penetrates the atmosphere and heats earth's surface. 2. objects on earth's surface emit long wavelength radiation skyward 3. greenhouse gases absorb outgoing, long wavelength radiation and radiate some of this energy earthward, thus trapping heat in the lower atmosphere. |
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The Recent Past (60 years) |
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The concentration of carbon dioxide has increased steadily since 1958 with smaller, annual variations |
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The longer trend shows increasing carbon dioxide concentrations: |
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Increasing CO2 from burning of fossil fuels |
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Temperatures have also increased over the last 50 years!.... |
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BUT is the temperature increase related to the increase in CO2? |
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Large temperature changes have also occurred in the geologic past, so it is not clear! |
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Global temperatures during the Middle Cretaceous and Early Cenozoic were higher than today |
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Temperature changes over the last few thousand years must be obtained indirectly in what are known as proxy recorders: – Trapped atmospheric gases in ice cores – Oxygen isotope changes in ice cores – Oxygen isotope and other changes in fossils in oceans and lakes |
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Earth today is close to equaling the highest average temperature of the |
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Climatic Models And Future Temperatures |
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Predicting The Extent And Consequences Of Global Warming |
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General Circulation Model |
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Scientists developed a complex computer climate model known as a General Circulation Model (GCM) |
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A GCM contains several sub-model programs for the following: |
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Atmosphere – Ocean – Land surface – Cryosphere – Biosphere |
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Variables in GCMs include the following: |
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– Temperature – Precipitation – Air Pressure – Relative Humidity – Wind – Sunlight intensity |
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GCMs calculate scenarios of |
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future climate change based on input parameters and variables |
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A General Circulation Model consists of a |
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grid of boxes, each representing a different location on Earth; Each box consists of multiple layers and interacts with adjoining boxes |
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Overall Effects Of Climate Change |
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Center is climate change. a) risks to unique and threatening systems. b) risks of extreme weather events c) uneven distribution of climate change impacts d) aggregate impacts and damages e) risks of large scale discontinues and disruptoirs |
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a) risks to unique and threatening systems. |
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Loss of glaciers (global warming), coral reefs (ocean acidification), barrier islands and small islands (rising sea level): ecosystems migrate and species become extinct
Melt-water from melting glaciers flow into the oceans, causing sea level to rise |
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e) risks of large scale discontinues and disruptoirs |
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Dynamic equilibrium is disrupted, tipping point is reached and the system spasms to a new equilibrium state: disruptions include melting of mountain and continental glaciers, sea-level rise, and ocean acidification
Oceans acidify due to absorption of increasing amounts of atmospheric CO2 |
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d) aggregate impacts and damages |
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Climate change results in monetary damage due to crop failures and diminishing water supplies: lives are changed or lost; poorer countries might not adapt successfully |
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b) risks of extreme weather events |
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Magnitude and frequency of extreme weather events increase: precipitation and floods intensify: hurricane and tornado intensities increase: more heat waves, droughts, and wildfires |
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c) uneven distribution of climate change impacts |
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Impacts are greatest in lowlatitude and lessdeveloped countries due to shifts in crop patterns and spread of diseases. At high latitudes, indigenous people of the circumpolar Arctic will be affected by rapid melting of ice sheets/permafrost. |
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Which of the following processes LEAST-LIKELY influence Earth's climate system? |
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Which of the following tropical climates receives the LEAST amount of annual rainfall? |
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A continental-arctic (cA) air mass that is very cold and dry would most-likely be characterized by a ___________ climate. |
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Most of the Gulf coastal region, including Houston, is characterized by a ____________ climate |
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The climograph below most likely reflects a ____________ climate |
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The climograph below most likely reflects a _________ climate. |
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Which of the following is NOT associated with El Nino? |
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Increased upwelling of deep ocean water along the west coast of South America |
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Which of the following satellite images depicts La Nina? Note that the white and red colors indicate warmer surface water while purple and blue indicates cooler surface water. |
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greens, yellows are everywhere, and the middle is purple and blue. it's to the west of the americas but near the equator. |
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The following computer models calculate future rates of global warming based on our continued use of _____________. |
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Climatologists attempt to predict future climate changes using __________ |
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. Computer models known as General Circulation Models |
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