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: “Thursday morning is damp for some, but for most it's a fine day. We are chasing clouds. There will be some brightness in the sky as well. There’s low pressure sitting towards the north of Scotland, hence the reason why it has been rather windy and gusty across Scotland and in fact cloud and rain
: “Thursday morning is damp for some, but for most it's a fine day. We are chasing clouds. There will be some brightness in the sky as well. There’s low pressure sitting towards the north of Scotland, hence the reason why it has been rather windy and gusty across Scotland and in fact cloud and rain
Tropical Storm Outlook 10 Vertical Wind Shear Vertical wind shear is a measure of the variation of the horizontal wind with height. In this instance the shear is measured between the 200 hPa and 850 hPa pressure surfaces. Low values of vertical wind shear, typically below 10ms -1 , are considered
traditional meteorological sites, satellite earth observation (EO) systems, weather balloon systems, and the UK radar network. The Met Office also collects data on air conditions, soil, relative humidity, wind speed, atmospheric pressure, sea surface temperature, sea ice, as well as a range of other
flows along the coast of Ecuador and Peru, disrupting the local fishery. It has since become identified with warming of the tropical Pacific Ocean east of the dateline. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called
. This oceanic event is associated with a fluctuation of a global-scale tropical and subtropical surface pressure pattern called the Southern Oscillation. This coupled atmosphere–ocean phenomenon, with preferred time scales of two to about seven years, is known as the El Niño-Southern Oscillation (ENSO
is relative humidity at the surface, huss is specific humidity at the surface, psl is sea level pressure, rls is the long wave radiation at the surface, rss is the short wave radiation at the surface, sfcWind is wind speed at 10m, tas is mean temperature at the surface, tasmin is minimum temperature
region were indeed neutral (i.e. tropical Pacific sea surface temperatures, sea level pressure, cloudiness and trade winds indicated that neither El Niño nor La Niña conditions were present; WMO 2013). Furthermore, cool SST anomalies were also present in the far eastern Pacific, although they were
29.5 16.9 791 11 129 29 HadCM3Q11 0.967986 29.6 17.4 837 8 133 29 IMD observed (1975-2005) 30.9 18.6 863 12 119 28 variables are surface pressure, zonal and meridional wind components, potential temperature and cloud-conserved temperature, and moisture at the 19 levels of atmosphere. A relaxation
between June-September. ENSO involves recurrent changes in sea surface temperatures and atmospheric surface pressure across central and eastern tropical Pacific. ENSO has three phases: El Niño, La Niña, and neutral. El Niño generally suppresses monsoon rainfall while La Niña generally increases
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