In a post last week, «
Warm winds slow autumn ice growth,» NSIDC noted «October 2009 had the second - lowest ice extent for the month over the 1979 to 2009 period.»
Not exact matches
In some places the season got off to a
slow start due to unusually
warm weather, but where early frosts and high
winds got the birds off their tails excellent shooting was reported.
«I am very interested in these
wind speed increases and whether they may have also played some role in
slowing down the
warming at the surface of the ocean,» said Prof Sherwood.
The wedge strategies rely on existing technologies such as
wind power and fuel - efficient vehicles, so the activity drives home the hopeful message that we already have tools to
slow global
warming.
• Clouds form because cold air doesn't hold as much water as
warm air • Clouds are made of water vapor • Clouds always predict rain • Rain falls when clouds become too heavy and the rain drips out or bursts the cloud open • Rain comes from holes in clouds, sweating clouds, funnels in clouds, melted clouds • Lightning never strikes the same place twice • Thunder occurs when two clouds collide • Clouds block
wind and
slow it down • Clouds come from somewhere above the sky • Clouds are made of smoke How does the 5E model facilitate learning?
My own view is, (a) if we
wind up at the lower end of the IPCC expected
warming, maybe we shouldn't be spending large sums to avert it, whereas if we are likely to land at the high end, the costs miht start to get fairly grave (b) nobody has a very good idea how much it would really cost to avert, or
slow, global
warming (hope this doesn't contradict (a)-RRB-.
Simple physics dictates that with less sea ice there is magnified
warming of the Arctic due to powerful albedo feedback; this in turn reduces the equator to pole temperature gradient which
slows the jet stream
winds causing them to become more meridional; this combined with 4 % more water vapor in the atmosphere (compared to 3 decades ago) is leading to much more extremes in weather.
Another riddle was that previous research indicated that under global
warming scenarios Pacific Equatorial Trade
winds would
slow down over the coming century.
The article found current CO2 emissions aren't falling rapidly enough to
slow global
warming largely because most public policy has focused exclusively on developing
wind and solar power, which may actually increase emissions.
Slower winds could create wilder swings of the jet stream, allowing
warm, moist air to penetrate farther north.
It wasn't that long ago the story was global
warming was
slowing trade
winds.
Now the story is trade
winds are
slowing global
warming.
El Niño - Pacific Ocean trade
winds slow and almost stop which brings
warmer conditions and weak upwelling currents to the eastern Pacific which hurts fishing in Peru
Some of the
warm water would be subducted by Atlantic Meridional Overturning Circulation / Thermohaline Circulation, some would be carried by ocean currents into the Arctic Ocean where it would melt sea ice, and the remainder would be spun southward by the North Atlantic gyre toward the tropics so it could be
warmed more by the effects of the
slower - than - normal trade
winds.
Much of it is forced down and it flows back to the east at 200 metres depth and when the
warm water surfaces at the Galapogos Islands in 9 months (replaceing the water which is flowing east - west at the surface), it starts to
slow down the Trade
Winds because of the convection effect.
And since the temperature difference between the Arctic and the tropics is narrowing, and since it's the temperature difference that drives
wind and ocean currents, then the jet stream that normally whizzes around the Arctic circle — thus keeping frozen air in one place and separating it from the
warm breezes of the south — is, the theory goes,
slowing, thus allowing
warm moist air to penetrate into the north.
Wouldn't it be ironic if in the interest of global
warming we mandated massive switches to energy, which is a finite resource, which
slows the
winds down, which causes the temperature to go up?
CO2, if it had any affect on trade
wind speed should lead to the East to West trade
wind speed
slowing down, thus setting up the Pacific oscillation to its
warm El Nino conditions as the predominant condition.
The normally west - to - east
winds suddenly
slowed and switched direction completely as the stratosphere rapidly
warmed more than 50 degrees F in a matter of days (see figure below).
According to data from the Ocean Surface Topography Mission / Jason 2 satellite, ocean temperatures in the central and eastern equatorial Pacific are significantly
warmer than usual due to
slowing trade
winds.
Additional heat released to the atmosphere from the opening ocean will amplify the Arctic
warming and generate atmospheric waves which ultimately
slow down stratospheric
winds.
To summarise the arguments presented so far concerning ice - loss in the arctic basin, at least four mechanisms must be recognised: (i) a momentum - induced
slowing of winter ice formation, (ii) upward heat - flux from anomalously
warm Atlantic water through the surface low ‐ salinity layer below the ice, (iii)
wind patterns that cause the export of anomalous amounts of drift ice through the Fram Straits and disperse pack - ice in the western basin and (iv) the anomalous flux of
warm Bering Sea water into the eastern Arctic of the mid 1990s.
This intensification of
winds initially triggers a rapid cooling of the sea surface and expansion of sea ice, but this is followed by a
slow process of
warming and sea ice contraction.
WHEN the skin layer is
warmer than the water below (and not mixed by the
wind), there is no obvious mechanism (other than very
slow conduction) for AGG - enhanced DLR to penetrate the ocean.
«Recent research, however, suggests that there is a possibility that this gradual global
warming could lead to a relatively abrupt
slowing of the ocean's thermohaline conveyor, which could lead to harsher winter weather conditions, sharply reduced soil moisture, and more intense
winds in certain regions that currently provide a significant fraction of the world's food production.
Enhanced
warming of the Arctic affects the jet stream by
slowing its west - to - east
winds and by promoting larger north - south meanders in the flow.
Whilst largely unanticipated in the climate change impacts community, previous analyses have predicted a
slowing in the overall circulation rate in tropical regions and, presumably, a reduction in averaged
wind speed in those regions with greenhouse
warming [Betts, 1998; Held and Soden, 2006; Vecchi et al., 2006].............
We know what burning fossil fuels does to
warm the planet, but now research is showing that air pollution is actually
slowing down
wind speeds, hampering the effectiveness of
wind farms themselves.
A statewide Renewable Energy Standard (RES), a requirement that utilities obtain a percentage of their power from renewable resources like
wind, would keep Missouri thriving economically and doing its part to
slow global
warming.
The North Atlantic
warms in a few months in response to an El Niño, through changes in atmospheric circulation (
slower trade
winds in the tropical North Atlantic, for example).
The researchers are interested in exploring these increases in
wind speed to determine if they have a role in
slowing down
warming in ocean surfaces.
Evergreen shrubbery around the house foundation helps keep the house
warmer in winter by
slowing down the
wind; and cooler in summer.