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En Route Weather Depiction Benefits of the NEXRAD Vertically
En Route Weather Depiction Benefits of the NEXRAD Vertically

... eventually benefit from DQA as well, but must wait until its NEXRAD ORPG release for incorporation into its system. ...
5.2 EN ROUTE WEATHER DEPICTION BENEFITS OF THE NEXRAD VERTICALLY
5.2 EN ROUTE WEATHER DEPICTION BENEFITS OF THE NEXRAD VERTICALLY

... eventually benefit from DQA as well, but must wait until its NEXRAD ORPG release for incorporation into its system. ...
Introduction on Supercells
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... The updraft is the rising column of air in the supercell  They are generally located on the front or right side of the storm  Entrainment is small in the core of the updraft  Updraft speeds may reach 50 m s-1!!!  Radar indicates that the strongest updrafts occur in the middle and upper parts of ...
some effects of the evaporation of widespread
some effects of the evaporation of widespread

... constitutes quite a departure from the ideas of the Nor- definition of fronts, since by definition a cold front lies at wegian school of air mass analysis, analysts were at first the forward edge of the transition zone, and such revision reluctant to accept it. Many forecasters still introduced null ...
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weather - Sikkim Springs
weather - Sikkim Springs

...  As the difference is so significant within such a small distances, there is a great need to have accurate data for a specific area of interest.  At government level, rainfall and evaporation data is available at taluka HQ which may not represent the actual value at the field.  Therefore such dat ...
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Weather forecasters predict a good season for Uganda
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Weather Unit 2
Weather Unit 2

... temperate to subtropical areas, often with cold winters and hot summers.  Found between deserts and forests  In the northern hemisphere the main grasslands are the prairies of the midwestern United States and Canada; in Eurasia the maker grasslands are the steppes of Russia and the grasslands of t ...
precipitation rain sleet hail
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... Severe weather events pose a direct threat to life, health, infrastructure, production and assets. Such threats are becoming increasingly severe due to increased urbanisation, population growth and climate change. Extreme and highly localised weather events are appearing more frequently, meaning sta ...
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4 October

... Inject cloud with small particles that act as ice condensation nuclei, starting the precipitation process. NEED CLOUDS: seeding does not generate clouds Cold clouds with a low seed ration best Dry ice, silver iodide ...
Quantifying the drivers of European precipitation changes: Large
Quantifying the drivers of European precipitation changes: Large

1

United States rainfall climatology



The characteristics of United States rainfall climatology differ significantly across the United States and those under United States sovereignty. Late summer and fall extratropical cyclones bring a majority of the precipitation which falls across western, southern, and southeast Alaska annually. During the winter, and spring, Pacific storm systems bring Hawaii and the western United States most of their precipitation. Nor'easters moving down the East coast bring cold season precipitation to the Carolinas, Mid-Atlantic and New England states. Lake-effect snows add to precipitation potential downwind of the Great Lakes, as well as Great Salt Lake and the Finger Lakes during the cold season. The snow to liquid ratio across the contiguous United States averages 13:1, meaning 13 inches (330 mm) of snow melts down to 1 inch (25 mm) of water.During the summer, the North American monsoon combined with Gulf of California and Gulf of Mexico moisture moving around the subtropical ridge in the Atlantic ocean bring the promise of afternoon and evening air-mass thunderstorms to the southern tier of the country as well as the Great Plains. Equatorward of the subtropical ridge, tropical cyclones enhance precipitation across southern and eastern sections of the country, as well as Puerto Rico, the United States Virgin Islands, the Northern Mariana Islands, Guam, and American Samoa. Over the top of the ridge, the jet stream brings a summer precipitation maximum to the Great Lakes. Large thunderstorm areas known as mesoscale convective complexes move through the Plains, Midwest, and Great Lakes during the warm season, contributing up to 10% of the annual precipitation to the region.The El Niño-Southern Oscillation affects the precipitation distribution, by altering rainfall patterns across the West, Midwest, the Southeast, and throughout the tropics. There is also evidence that global warming is leading to increased precipitation to the eastern portions of North America, while droughts are becoming more frequent in the western portions.
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