Teleconnection Map Climate teleconnections were first investigated in the sea-level pressure (SLP) field. SLP is however an ill-defined quantity over land, particularly near the mountains; it can moreover be influenced by local meteorological processes. Teleconnectivity is thus better analyzed in upper...
The 40-1/2 years of mean montly sea level pressure maps based on the Historical Map Series have been typed according to numerical indices that indicate to what extent each particular monthly map resembles a typical or normal winter or summer map on one hand, or a typical spring or fall ...
The 40-1/2 years of mean montly sea level pressure maps based on the Historical Map Series have been typed according to numerical indices that indicate to what extent each particular monthly map resembles a typical or normal winter or summer map on one hand, or a typical spring or fall map...
网络平均海面压力 网络释义 1. 平均海面压力 消防专业词汇英语翻译(H-O) ... mean of egress 疏散设施mean sea level pressure平均海面压力mean sea level 平均海平面 ... www.zftrans.com|基于18个网页 例句
Once in 50-year geostrophic wind speeds have been calculated for Europe using mean sea level pressure maps. The resulting wind speeds have then been converted to the equivalent 10-min mean surface wind speeds using the geostrophic drag law. Surface wind speeds are found to be in good agreement...
We have computed seasonal harmonics of the IB from ERA5 (mean sea level) pressure data for the period 1993–2017. The calculation accounts for variations in the mean pressure over the global ocean, which is predominantly an annual variation of mean amplitude approximately 0.6 hPa, maximum in Ju...
Because the future global sealevel rise, if real, will exert a great impact on the coastal environment, the Chinese scientists have shown great interests in the sealevel changes along the Shanghai coastal area where the natural environment and society are highly vulnerable to the sealevel changes...
(Fig.3c) that is consistent with zonal asymmetries in near surface temperature and sea level pressure response over regions of sea ice loss (Fig.1), but the main signal is an equatorward shift resulting in an increase inFparound 35–55∘N that also extends into the stratosphere. Hence, ...
It is well-known that, in the open ocean, much of the observed temporal variability in sea level can be accounted for by variations in density (steric sea level), effectively assuming no variability in ocean bottom pressure. However, this clearly cannot remain the case as the depth of the ...
Such retreat is likely to trigger extensive ice loss of the WAIS8,9, contributing as much as 3.4 m to global sea level over the next several centuries10. Fig. 1: Map of Amundsen Sea Embayment, Antarctica, showing sites mentioned in the text. Our study locations are shown in bold ...