Mid- Mid -latitude cycloneMeteorology, Satellite
网络中纬气旋;中纬度气旋 网络释义
METEOROLOGIST JEFF HABY A mid-latitude cyclone is a region of low pressure that often travels in connection with the jet stream. A mid-latitude cyclone is baroclinic which means it has fronts associated with it. There are three areas that they commonly develop which are land/sea boundaries, mo...
Sensitivity of US air quality to mid-latitude cyclone frequency and implications of 1980–2006 climate change. Atmos. Chem. Phys. 8: 7075 – 7086 .Leibensperger, E.M. Mickley, L.J. and Jacob, D.J. \Sensitivity of US air quality to mid-latitude cy- clone frequency and implications of...
Milankovich theory suggested that orbitally induced summer insolation change at high-latitude region of Northern Hemisphere played a key role in driving the ice cycles during the Pleistocene. However, a significant shift of the Pleistocence climate from 41-ka to 100-ka cycles (namely mid-Pleistocen...
South poleward migration 1° latitude (about 100 km) per decade (Kossin et al., 2014; Studholme et al., 2022) may increase cyclone frequency in the remote south-eastern Tuamotu region. However, with the projected expansion of the tropical climate zone, there will have a potential ...
The latitudinal temperature gradient between the Equator and the poles influences atmospheric stability, the strength of the jet stream and extratropical cyclones1,2,3. Recent global warming is weakening the annual surface gradient in the Northern Hemisphere by preferentially warming the high latitudes4;...
However, the magnitude of the warming in the mid- to high-latitude North Atlantic, in both DMMM and any DMODEL , is small compared to DPRISM. While the variability of DPRISM (a function of the within-time-slab variability at those localities) and the spread of the individual DMODEL ...
middle latitude cyclones Large centers of low pressure that generally travel from west to east and cause stormy weather. Step 1 Large air masses with different densities meet.cP and mT Step 2 The boundary between the two air masses takes on a wave shape. Step 3 Warm air advances poleward ...
This suggests that the mean GrIS 2m-temperature depends more on the height of the 500 hPa-(anti)cyclone at the centre of the ice sheet than on its precise location and pattern. Thus, contrary to Lund (1963), the Z 500 surface height takes a larger part in our CTC (via the similarity...