Naturally many factors
influence polar sea ice extent, such as weather patterns, winds, -LSB-...]
Naturally many factors
influence polar sea ice extent, such as weather patterns, winds,
Not exact matches
Oceanography postgraduates, for example, might study how coastal dynamics affect amphibious warfare, or how decreasing
polar sea ice might
influence global climate patterns.
«With most [species], we can identify a localized threat, but the threat to the
polar bear comes from global
influences on
sea ice.»
The newly discovered phenomenon over the South
Seas boosts ozone depletion in the
polar regions and could have a significant
influence on the future climate of Earth — also because of rising air pollution in South East Asia.
Sea ice is a crucial part of the ecosystems at both poles, providing habitat and
influencing food availability for penguins,
polar bears and other native species.
The strength of these currents is
influenced by the location of the
polar fronts as determined by
sea level pressures in the Southern and Northern Annular Modes.
««In terms of the human
influence on the Antarctic, I think you have to be very cautious about over-interpreting the results of the paper, that's the bottom line,» added Eric Rignot, a
polar researcher with NASA and the University of California - Irvine who published a blockbuster study on the destabilization of the Amundsen
Sea in 2014.»
Franz Josef Land provides the most stable
sea ice habitat for Barents Sea polar bears because it is largely beyond the influence of warm water influxes from the North Atlant
sea ice habitat for Barents
Sea polar bears because it is largely beyond the influence of warm water influxes from the North Atlant
Sea polar bears because it is largely beyond the
influence of warm water influxes from the North Atlantic.
Screen (32) explored the
influence of Arctic
sea ice on European summer climate using a state - of - the - art atmospheric model in view of the historically unprecedented sequence of six consecutive wet summers from 2007 to 2012 in northern Europe, which featured a marked southward shift of the
polar jet stream.
Factors like ENSO, the MJO,
sea ice, snow cover, and oscillations in the tropical stratospheric winds have all been found to
influence the strength of the
polar vortex.
This in turn is
influenced by
sea level pressure patterns in
polar and subpolar regions — as more or less wind and currents are pushed north (Roemmich et al, 2007, Qiu, Bo et al 2006).
You say anthropogenic
influences on
polar sea ice is not a difficult concept to understand.
Now, finally, to «the faith of the
polar bear» — a species like any other,
influenced by a myriad of environmental factors, including bullets and melting
sea ice
In its first comprehensive report since winning a Nobel Peace Prize in 2007, the IPCC is unequivocal about the
influence of human activity, the progressive warming of the planet, the melting of the
polar ice caps, and the rise in
sea level.
While climate change does not affect Earth's tilt, it does have potential implications for many of the other factors that
influence winter weather in the US, including Arctic
sea ice, the
polar jet stream, the
polar vortex, and El Niño.
Features of the model described here include the following: (1) tripolar grid to resolve the Arctic Ocean without
polar filtering, (2) partial bottom step representation of topography to better represent topographically
influenced advective and wave processes, (3) more accurate equation of state, (4) three - dimensional flux limited tracer advection to reduce overshoots and undershoots, (5) incorporation of regional climatological variability in shortwave penetration, (6) neutral physics parameterization for representation of the pathways of tracer transport, (7) staggered time stepping for tracer conservation and numerical efficiency, (8) anisotropic horizontal viscosities for representation of equatorial currents, (9) parameterization of exchange with marginal
seas, (10) incorporation of a free surface that accommodates a dynamic ice model and wave propagation, (11) transport of water across the ocean free surface to eliminate unphysical «virtual tracer flux» methods, (12) parameterization of tidal mixing on continental shelves.