But maps
of sea level pressure can also be averaged over several months or years, to show the average circulation patterns in the atmosphere.
The measurement isn't exclusive to dog bite strength, it's used to measure everything from the pressure in a bike tire to the
atmospheric sea level pressure.
The weight of the atmosphere's water vapor contributes only about one quarter of one percent of the
total sea level pressure of all the gases.
Other climate or climate - related variables of importance may include CO2 concentration, sea - ice extent,
mean sea level pressure, sea level, and storm surge frequencies.
Conversely, low
sea level pressure anomalies over the Beaufort Sea and Canada Basin keep the Arctic Ocean pack ice up against the western entrance.
Closed contours over the Pacific Arctic support a continued
low sea level pressure in that region, similar to Figure 9, which is not supportive of rapid sea ice loss.
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).
However, unusually
high sea level pressure centered over northern Scandinavia brought southerly winds from the East Siberian and Barents Seas, contributing to high air temperatures in these regions.
As there are numerous techniques for determining
sea level pressures from atmospheric observations, all having limitations, we also compared the SLP fields generated in the above way for general consistency with those generated using an independent method.
A measure of the difference in
sea level pressure between the western (e.g., Darwin, Australia) and central / eastern (e.g., Tahiti) equatorial Pacific, representative of the east - west changes in atmospheric circulation associated with the El Nino / Southern Oscillation phenomenon.
In central North America, the cooler winters were primarily due to changes in the northerly winds driven by increased
sea level pressure on the west coast of North America.
This AD pattern quickly shifted in the second half of June 2012, however, and was replaced by a more typical low
sea level pressure center over the Arctic Ocean.
Variability in
sea level pressure decreases on average in the Southern Hemisphere, while in the Northern Hemisphere there are regional differences.»
The station component is a blend of many national and international collections, with the largest contributor being surface and
sea level pressure observations from the International Surface Database -LRB-
The map of
sea level pressure for October 1 to 30, 2010, shows a high - pressure system cenetered over the Beaufort and Chukchi sea and Greenland, and low pressure over the Kara and Barents seas.
Petrich (University of Alaska Fairbanks); 4.0 Million Square Kilometers with a Possible Range of 3.4 to 5.4 Million Square Kilometers, Likely Range of 3.4 to 4.9 Million Square Kilometers; Heuristic, Statistical Estimate is unchanged from last month and is based on the relationship between
June sea level pressure (SLP) and both surface winds and clouds, which are known to drive arctic sea ice reduction in summer.
The causal link between this aspect of solar activity and climate seems as nebulous as solar UV / ozone interactions in the stratosphere
driving sea level pressure at the poles.
In addition to incorporating data on October Eurasian snow cover extent, sea surface temperature, other inputs into the forecasts include anomalies from the fall season such
as sea level pressure anomalies and sea ice concentration anomalies.
Twice -
daily sea level pressure fields, gridded to 2 ° × 2.5 ° (lat × lon), are calculated using the method recommended by the NCEP Reanalysis project, which employs the 1000 HPa (z1000) and 500 HPa (z500) geopotential height fields in the following formula:
A new study in Geophysical Research Letters uses historical climate model simulations to demonstrate that there has been an Arctic - wide decrease in
sea level pressure since the 1800's.
Some work by Clara Deser et al. shows that for some diagnostics (e.g.,
regional sea level pressure 50 - yr trends, wintertime western U.S temperature, etc) that the sensitivity of trends in their decadal statistics to initial conditions can compete with the sensitivity of those same statistics in responses to increases in GHGs.
This updated dataset includes more data sources than the HadSLP v1.0 and is updated to April 2006, this dataset is documented in an upcoming J. Climate manuscript (Allan, R. and T. Ansell: A new globally - complete monthly historical gridded mean
sea level pressure data set (HadSLP2): 1850 - 2004.
An exception to this last statement is the slight increase in mean RMS error for
sea level pressure found in non-flux-adjusted models.
Phrases with «sea level pressure»