Not exact matches
Professor Baldwin added: «Natural large pressure fluctuations in the
polar stratosphere tend to last a long time — at least a month, and we see this reflected as
surface pressure
changes that look very much like the North Atlantic Oscillation — which has significant effects on weather and extreme events across Europe.»
As
changes happen in the
polar regions, they are carried around the world by ocean currents, both at the
surface and in the deep ocean.
The study simply wasn't aimed at identifying any causes of mass loss — it merely observed these losses using NASA's twin GRACE satellites, which measure mass and gravitational
changes at the Earth's
surface, and tied them to the resulting
polar motion.
Multiyear records of remotely sensed tDOM distributions provide direct evidence of how the routing, inventory, storage and residence time of tDOM in
surface polar waters
change in response to climatic forcing.
By facilitating the real - time, synoptic monitoring of tDOM and freshwater runoff in
surface polar waters, this novel approach will help understand the manifestations of climate
change in this remote region.
Although there is still some disagreement in the preliminary results (eg the description of
polar ice caps), a lot of things appear to be quite robust as the climate models for instance indicate consistent patterns of
surface warming and rainfall trends: the models tend to agree on a stronger warming in the Arctic and stronger precipitation
changes in the Topics (see crude examples for the SRES A1b scenarios given in Figures 1 & 2; Note, the degrees of freedom varies with latitude, so that the uncertainty of these estimates are greater near the poles).
Aren't those cyvlones not only steadily tugging more on the earth's
surface on our seas (e. g. the so - called monsterwaves) but pulling also on our firm crust in certain places, thereby provoking unusual outbreaks of volcanoes, like in Iceland, and with that maybe also causing every more a little
change on the
polar axis of our planet?
There are three large average
surface wind patterns few know about: the tropical easterlies (tradewinds), the midlatitude westerlies and the
polar easterlies, but variability results in significant weather
changes.
When
polar ice melts the earth
changes shape: mass (ice) which was concentrated at the poles, with a short arm of inertia, is spread evenly around the ocean
surface, averaging something like 63 degrees latitude.
More or less upwelling in the eastern Pacific is linked to
changes in wind and gyre circulation — in both hemispheres — driven by
changes in
surface pressure in the
polar annular modes.
AGW climate scientists seem to ignore that while the earth's
surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take water vapor scavenged from the vast oceans on earth (which are also a formidable heat sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of heat from the atmosphere) or freeze it, (removing even more vast amounts of heat from the atmosphere) drop it on land and oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the oceans and building
polar ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space,
changing the moment of inertia of the earth by removing water mass from equatorial latitudes and transporting this water vapor mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..
Because the GISS analysis combines available sea
surface temperature records with meteorological station measurements, we test alternative choices for the ocean data, showing that global temperature
change is sensitive to estimated temperature
change in
polar regions where observations are limited.
The puzzle of a shared 20 to 30 year pulse in both hemispheres is traced mechanistically back to
changing polar surface pressure fields — influencing storm tracks in high latitudes.
Storms and cloud spinning off the
polar vortices into lower latitudes — the
changes in sea
surface temperature over vast areas of the Pacific.
Also, as far as temperature
changes across the year are concerned, in the
polar regions right at the
surface, the main warming will be in the winter months.
As the
polar ice caps grow or melt, the
surface area of the earth covered by land relative to that covered by water
changes.
The
changes in the solar magnetic field impacting the Earth at
polar regions cause
changes in
surface pressure.
The more recent suggestion is that it is triggered by
changes in
polar surface pressure which modulate wind and ocean currents in both the north and south hemispheres.
Climate forcings due to past
changes in GHGs and
surface albedo can be computed for the past 800000 years using data from
polar ice cores and ocean sediment cores.
As the Earth's
surface cools further, cold conditions spread to lower latitudes but
polar surface water and the deep ocean can not become much colder, and thus the benthic foraminifera record a temperature
change smaller than the global average
surface temperature
change [43].
Furthermore warm ocean
surfaces really do send the air circulation systems poleward whilst
changes in the intensity of the
polar high pressure cells work in opposition to those oceanic effects.
In accordance with that proposition the ocean
surface temperatures
change cyclically and the
polar atmospheric oscillations
change cyclically.