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
Results 1-5 of 19
Page 3
... over- all production in marine ecosystems , including re- duced fisheries . Such decreases in productivity may be occurring off the California coast , where scien- tists have documented a measurable decrease in the abundance of 3.
... over- all production in marine ecosystems , including re- duced fisheries . Such decreases in productivity may be occurring off the California coast , where scien- tists have documented a measurable decrease in the abundance of 3.
Page 4
... decrease in the abundance of zooplankton , the second level in the food web . Currently the abundance of zoop ... decreasing thermohaline cir- culation . Recent evidence has demonstrated that freshwater influx from melting sea ice can ...
... decrease in the abundance of zooplankton , the second level in the food web . Currently the abundance of zoop ... decreasing thermohaline cir- culation . Recent evidence has demonstrated that freshwater influx from melting sea ice can ...
Page 5
... decreased on some reefs , and predict that calcification could decrease 17 to 35 % from pre - industrial levels by 2100. Re- duced density , combined with increased storm ac- tivity caused by global climate change and mass mortality of ...
... decreased on some reefs , and predict that calcification could decrease 17 to 35 % from pre - industrial levels by 2100. Re- duced density , combined with increased storm ac- tivity caused by global climate change and mass mortality of ...
Page 6
... decreased at a site in Monterey Bay over a 60 - year period coincident with warming sea temperatures . Studies of rocky reef fishes in the California Bight show that the proportion of northern species de- clined , while that of southern ...
... decreased at a site in Monterey Bay over a 60 - year period coincident with warming sea temperatures . Studies of rocky reef fishes in the California Bight show that the proportion of northern species de- clined , while that of southern ...
Page 10
... decreased by 0.02 ° C per century for the 900 years previous to the 20th century . But beginning around 1900 this cooling trend was reversed in less around 1900 this cooling trend was reversed in less ice sheet hasn't yet played much of ...
... decreased by 0.02 ° C per century for the 900 years previous to the 20th century . But beginning around 1900 this cooling trend was reversed in less around 1900 this cooling trend was reversed in less ice sheet hasn't yet played much of ...
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.