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OMAHA — Every four years, the United States Olympic swimming trials sweep through the sporting landscape like a fast-moving weather front, bearing fickle winds of fate, thundering performances and heavy precipitation in the form of tears.
Winter in the maritime Arctic (the Aleutians, coastal southwestern Greenland, Iceland, and the European Arctic) is a period of storminess, high winds, heavy precipitation in the form of either snow or rain (the latter at sea level), and moderate temperatures.
Stretch the metaphor a little and space even possesses something a little like precipitation, in the form of clouds of dust and rock that we see from Earth as meteor showers.For almost all of history, space weather was a mysterious, occasionally pretty irrelevance.
Extreme precipitation in the form of heavy rain or snowfall is mostly triggered through convective (cumulonimbus) clouds.
It was found that defluoridation from water occurred due to adsorption by bleaching powder and slightly due to precipitation in the form of calcium fluoride.
Since the draft indicator did not register any precipitation, it is possible that precipitation in the form of small snowflakes had a weak effect.
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Overall discharge from the upper catchment is affected by a combination of runoff from glacier melt, changes in total precipitation, changes in the form of precipitation from snow to rain, seasonal changes in precipitation, and changes in net runoff.
Precipitation, usually in the form of light showers, is slight.
The mountainous region of the upper Indus receives precipitation largely in the form of snow.
High in the 2,000-metre-plus 2,000-metre-plus 2,000-metre-plusrecipitatiOlympics in the formountains, which feeds much than 250 glaciers, making this the mofthataciated US terrain outside Alaska.
Annual precipitation, mostly in the form of snow, varies from 16 inches (400 mm) in the north to 24 inches (600 mm) in the south, with snow cover in the Ladoga region accumulating to 40 inches (1,000 mm).
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deposition in the form of
occurrence in the form of
storm in the form of
climate in the form of
phenomenon in the form of
rain in the form of
fallout in the form of
season in the form of
water in the form of
pace in the form of
precipitation in the region of
precipitation in the presence of
precipitation in the bulk of
precipitation in the study of
precipitation in the watershed of
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