The disappearance of the polar ice cap could also
affect global ocean circulation patterns, and its melting has already imperiled native species such as the polar bear.
Scientists believe that the depth at which meltwater enters the ocean can
affect global ocean circulation and, in turn, climate.
«Melting Greenland ice sheet may
affect global ocean circulation, future climate: University of South Florida and international scientists find influx of freshwater could disrupt the Atlantic Meridional Overturning Circulation, an important component of global ocean circulation.»
Not exact matches
Gross says that the most important processes
affecting day length are changes in the weather, especially unusual variations in the strength and direction of the winds, which bring on alterations in the
global circulation of the atmosphere and
ocean.
«If these waters no longer sink, it could have far reaching
affects for
global ocean circulation patterns.»
Glacial retreat
affects ocean circulation patterns, fisheries and
global sea level rise.
Changes in the Arctic
affect the rest of the world, not only in obvious ways (such as the Arctic's contribution to sea - level rise), but through the Arctic's role in the
global climate system, its influence on
ocean circulation, and its impacts on mid-latitude weather.
Scientists also think that the
circulation of heat from the top layers of the
ocean, which have been most
affected to date, to the deeper
oceans below may be another factor behind the «hiatus» in
global warming.
The Antarctic ice sheet reached the coastline for the first time at ca. 33.6 Ma and became a driver of Antarctic
circulation, which in turn
affected global climate, causing increased latitudinal thermal gradients and a «spinning up» of the
oceans that resulted in: (1) increased thermohaline
circulation and erosional pulses of Northern Component Water and Antarctic Bottom Water; (2) increased deep - basin ventilation, which caused a decrease in oceanic residence time, a decrease in deep -
ocean acidity, and a deepening of the calcite compensation depth (CCD); and (3) increased diatom diversity due to intensified upwelling.
«The authors write that North Pacific Decadal Variability (NPDV) «is a key component in predictability studies of both regional and
global climate change,»... they emphasize that given the links between both the PDO and the NPGO with
global climate, the accurate characterization and the degree of predictability of these two modes in coupled climate models is an important «open question in climate dynamics» that needs to be addressed... report that model - derived «temporal and spatial statistics of the North Pacific
Ocean modes exhibit significant discrepancies from observations in their twentieth - century climate... conclude that «for implications on future climate change, the coupled climate models show no consensus on projected future changes in frequency of either the first or second leading pattern of North Pacific SST anomalies,» and they say that «the lack of a consensus in changes in either mode also
affects confidence in projected changes in the overlying atmospheric
circulation.»»
That is because there are factors, like air and
ocean circulation patterns, that
affect both the rate and the intensity of the
global warming.
Opening of the Drake Passage surely
affected ocean circulation around Antarctica, but efforts to find a significant effect on
global temperature have relied on speculation about possible effects on atmospheric CO2 [37].
Sea ice can strongly
affect global systems, influencing
ocean circulation patterns, levels of reflected radiation (10, 11), and rates of climate change (12).
From a report described on the IPY (International Polar Year) site dated 2/25/09: «Snow and ice are declining in both polar regions,
affecting human livelihoods as well as local plant and animal life in the Arctic, as well as
global ocean and atmospheric
circulation and sea level.»
«Greenland hosts the largest reservoir of freshwater in the northern hemisphere, and any substantial changes in the mass of its ice sheet will
affect global sea level,
ocean circulation and climate,» said Velicogna.
Researchers also knew that
global circulation patterns in the
oceans — patterns caused mostly by variations in water temperature and saltiness —
affect global climate.