precipitable water vapor oor Spaans

precipitable water vapor

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agua precipitable

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He considered pseudo-adiabatic processes describing air as it is lifted, expands, cools, and eventually condenses and precipitates its water vapor.
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When these transitions are reversed (that is, when water freezes or vapor precipitates) heat is released.
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Water vapor in the clouds condenses and precipitates as rain, which “saturates the earth.”
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As the water vapor rises and cools, it condenses, until it returns to Earth as precipitation.
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WP4 Estimation of the contribution of vegetal cover evapotranspiration to the precipitable water vapor recharge within the diurnal breeze circulations along the Turia river valley.
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As we know from science, rain is liquid water in the form of droplets which have condensed from atmospheric vapor and then precipitated.
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When a telescope needs to occupy an area that covers many square kilometers and must be located above most of the precipitable water vapor in the atmosphere, there aren’t many places left to choose from.
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Microwave Remote Sensing: Clouds, Precipitation, and Water Vapor
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Something like 20 billion tons per day of water vapor is sucked up by the northeastern trade winds, and eventually precipitates in the form of rain across the La Plata Basin.
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Precipitation: change of water vapor to liquid water.
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Advanced satellite products, including Integrated Water Vapor and Total Precipitable Water, provide excellent observations of AR development and evolution.
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All freshwater ultimately comes from precipitation of atmospheric water vapor, reaching inland lakes, rivers, and groundwater bodies directly, or after melting of snow or ice.
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The generated water vapor condenses thereby forming a suspension of fresh water droplets inside a chamber till the fresh water suspension is evacuated from the environmental space to containers prepared to receive the droplets and where the suspension precipitates in order to collect the resulting fresh water flow.
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Presently the atmosphere becomes sufficiently cool to cause condensation of the water vapor and precipitation of rain upon the hot rocks.
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Climate; Climatic change; Global change; Model; Atmospheric moisture; Water vapor; Isotope analysis; Precipitation; Convection; Classification code(s)
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Consequently, the concentration of atmospheric water vapor, which determines the water for precipitation, is substantially increasing in accordance with the Clausius-Clapeyron (CC) relationship, which establishes that water vapor in the atmosphere increases at a rate of 7% peroC of warming.
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Evaporation exceeds precipitation over the oceans, and this water vapor is transported by the wind over land, where it returns to the land through precipitation.”[2]
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Between 15° and 20°S precipitation is negatively associated to water vapor advection from the ocean, i.e. it rains when humidity is transported from the continent.
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Globally, about two-thirds of this precipitation returns to the atmosphere as water vapor, and the majority of that falls again on land.
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Rainfall and snowfall are generally slight due to the low vapor pressure of water in the chilly atmosphere, but as a rule potential evapotranspiration is extremely low, allowing soggy terrain of swamps and bogs even in places that get precipitation typical of deserts of lower and middle latitudes.
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Precipitation is the product of condensation of atmospheric water vapor.
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Areas of lower humidity cause the preferential loss of 18O water in the form of vapor and precipitation.
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As the air rises, water vapor condenses into clouds that can bring precipitation.
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Water vapor is most important from the meteorological point of view because it produces condensation and precipitation, forming clouds, rain, dew, snow, etc.. Water vapor also absorbs solar and terrestrial energy and serves as the principal source for developing storms and stabilizing the Earth's atmosphere.
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65 sinne gevind in 14 ms. Hulle kom uit baie bronne en word nie nagegaan nie.