Turning Up the Heat: How Global Warming Threatens Life in the SeaDIANE Publishing, 1999 - 47 pages Discusses current predictions of global climate change & synthesizes scientific evidence of the likely impacts of global climate change on some species & ecosystems. Chapters: global climate change & the oceans: sea level rise, wind patterns, deep-ocean circulation patterns, ocean stratification & primary productivity, & natural climate variability; lessons from El Nino & decadal variation; evidence of impacts on marine life: impacts in polar regions, coral reefs, shifts in species' distribution & the fate of Pacific Salmon, seabirds & marine mammals, & disease & harmful algal blooms; conclusion; & literature cited. |
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Page 10
... ( IPCC ) looks tinue at their present rate of increase ( IPCC 1990 ) . at what is likely to happen if CO , emissions con- A 1 % increase in CO , per year ( compounded ) will approximately 70 years , and quadruple the levels double the ...
... ( IPCC ) looks tinue at their present rate of increase ( IPCC 1990 ) . at what is likely to happen if CO , emissions con- A 1 % increase in CO , per year ( compounded ) will approximately 70 years , and quadruple the levels double the ...
Page 11
... ( IPCC 1995 ) . In their 1995 assess- ment , the IPCC concluded that , while our ability to quantify the human influence on global climate is limited by natural variability in part , " the bal- ance of evidence suggests that there is a ...
... ( IPCC 1995 ) . In their 1995 assess- ment , the IPCC concluded that , while our ability to quantify the human influence on global climate is limited by natural variability in part , " the bal- ance of evidence suggests that there is a ...
Page 12
... IPCC ( 1998 ) predicts a sea - level rise of 15-95 cm ( 6-37 inches ) by 2100 . The amount of sea level rise experienced by any Sea - level rise ( m ) 0.8 0.6 0.4 0.2 Total Thermal expansion Glaciers Greenland 0.0 Year 1900 2000 1950 ...
... IPCC ( 1998 ) predicts a sea - level rise of 15-95 cm ( 6-37 inches ) by 2100 . The amount of sea level rise experienced by any Sea - level rise ( m ) 0.8 0.6 0.4 0.2 Total Thermal expansion Glaciers Greenland 0.0 Year 1900 2000 1950 ...
Page 15
... for fishes and other populations , and hence for human consumption ( IPCC 1995 ) . Changes in species composition of phytoplankton populations may also enhance the buildup of CO2 2 in the atmosphere . For example , in the 15.
... for fishes and other populations , and hence for human consumption ( IPCC 1995 ) . Changes in species composition of phytoplankton populations may also enhance the buildup of CO2 2 in the atmosphere . For example , in the 15.
Page 19
... ( IPCC 1995 ; Hadley Centre 1998 ; Bering Sea Task Force 1999 ) . Since some climate change effects are likely to be seen first at higher latitudes , species in those areas may serve as an early warning system for changes to come ...
... ( IPCC 1995 ; Hadley Centre 1998 ; Bering Sea Task Force 1999 ) . Since some climate change effects are likely to be seen first at higher latitudes , species in those areas may serve as an early warning system for changes to come ...
Common terms and phrases
abundance Ainley Alaska algal blooms Antarctic Arctic areas Atlantic atmosphere Bering Sea biodiversity biological birds California Current carbon Cassin's auklets caused climate models coast coastal coccolithophores coral bleaching coral reefs crease decline decrease die-offs diseases effects environmental fish fisheries food web Fraser global change global climate change global temperatures Global Warming Threatens Glynn habitat Hadley Centre harmful algal blooms Heat How Global higher impacts intertidal invertebrates IPCC ISRS Kruse marine ecosystems marine mammals marine species mass mortalities mate change McGowan melting murres Niño events NOAA numbers nutrients occur ocean Pacific Salmon Pacific Seabird Group perature phytoplankton populations Press prey primary productivity rates recent reduced regions scientists sea ice sea level rise sea surface temperatures sea temperatures Seabird Group conference seabirds and marine seals shift sockeye Stirling stress surface waters tempera temperature increases thermohaline circulation tion toxic trend tropics tures Turning upwelling warm water warmer water temperatures zooplankton
Popular passages
Page 11 - Nevertheless, the balance of evidence suggests that there is a discernible human influence on global climate.
Page 35 - the balance of evidence suggests a discernible human influence on global climate...
Page 36 - STEVF.NINCK. 1984. Densities of the sea urchin Diadema antillarum before and after mass mortalities on the coral reefs of Curacao. Mar.
Page 38 - J. (1998). The relationship between increasing sea-surface temperature and the northward spread of Perkinsus marinus (Dermo) disease epizootics in oysters. Estuarine, Coastal and Shelf Science, 46, 587-97.
Page 22 - Satellite, operated and controlled by the National Oceanic and Atmospheric Administration (NOAA) of the US Department of Commerce, a satellite environmental data collection capability will become available to meet national requirements.
Page 38 - Simulated sea level change alters anatomy, physiology, growth, and reproduction of red mangrove (Rhizophora mangle L.). Oecologia...
Page 41 - W. Abdalati, E. Frederick, S. Manizade, C. Martin. J. Sonntag, R. Swift, R. Thomas, W. Wright, and J. Yungel (2000). Greenland Ice Sheet: High-elevation balance and peripheral thinning.
Page 36 - FP (1996). Primary productivity and its regulation in the equatorial Pacific during and following the 1991-1992 El-Nino, Deep-Sea Res.
Page 45 - Released by the Bureau of Oceans and International Environmental and Scientific Affairs, US Department of State, March 5, 1999.
Page 35 - ... [t]here is no known geologic precedent for the transfer of carbon from the Earth's crust to atmospheric carbon dioxide, in quantities comparable to the burning of fossil fuels, without simultaneous changes in other parts of the carbon cycle and climate system. This close coupling between atmospheric carbon dioxide and climate suggests that a change in one would in all likelihood be accompanied by a change in the other.