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. |
From inside the book
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Page 3
... Warm- ing sea surface temperatures can interfere with phytoplankton production by increasing stratifica- tion within the water column and increasing the thickness of the warm surface layer . Wind and upwelling will be less able to break ...
... Warm- ing sea surface temperatures can interfere with phytoplankton production by increasing stratifica- tion within the water column and increasing the thickness of the warm surface layer . Wind and upwelling will be less able to break ...
Page 4
... water near the poles sinks and moves toward the equator across the seafloor as warm water from the tropics moves poleward on the sur- face to replace it . This pattern of turnover in the oceans is called thermohaline circulation because ...
... water near the poles sinks and moves toward the equator across the seafloor as warm water from the tropics moves poleward on the sur- face to replace it . This pattern of turnover in the oceans is called thermohaline circulation because ...
Page 6
... warmer water and keeping up with this high me- tabolism requires large amounts of food . If suffi- cient food is not available , salmon can starve . Re- searchers predict that anticipated increases in wa- 4. Seabirds and marine mammals ...
... warmer water and keeping up with this high me- tabolism requires large amounts of food . If suffi- cient food is not available , salmon can starve . Re- searchers predict that anticipated increases in wa- 4. Seabirds and marine mammals ...
Page 11
... warm as any other cen- tury since 1400 AD , and that most climate studies ... warmest areas , while others may be limited by their dispersal abilities or ... water , melting of glaciers and the Greenland ice sheet , and melting of the ...
... warm as any other cen- tury since 1400 AD , and that most climate studies ... warmest areas , while others may be limited by their dispersal abilities or ... water , melting of glaciers and the Greenland ice sheet , and melting of the ...
Page 13
... warm faster than ever , studies at Blackwater Marsh on the Chesa- others . Accelerated warming of the planet surface ... Water Upland Blackwater National Wildlife Refuge 1980 - Surface Classification Trapping Unit Marsh Open Water Upland ...
... warm faster than ever , studies at Blackwater Marsh on the Chesa- others . Accelerated warming of the planet surface ... Water Upland Blackwater National Wildlife Refuge 1980 - Surface Classification Trapping Unit Marsh Open Water Upland ...
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.