www.travel-university.org

Atmospheric moisture

www.travel-university.org
Latest articles: Privacy - Sodertalje, Kebnekaise - Oland, Sodermanland - Boras, Trelleborg, Linkoping, Norrkoping - Gothenburg, Gotland - Lund, Jokkmokk, Jonkoping, Gota Kanal - Malmo, Lulea - Stockholm - Eskilstuna, Vattern, Vanern, Vasteras - Sweden at a Glance - Seasonal Lifestyle - Industrial Expertise - Farms and Mines - Forests and Lakes - Sweden
www.travel-university.org
Geography : Mineral Resources, Energy Resources, Universe, Structure of the Earth, Earth Layers, Earth Composition, Tectonics, Human Geography, Geomorphology, Oceanography, Cartography, History, Landforms, Climatology, Soils, Vegetation, Regions, Population, Resources, Industries,
Climatology: Air masses, Air pollution, Air temperature maps, Atmospheric moisture, Biochemical Cycle, Breezes, Climate change, Climates Classification, Clouds, Cyclones & Anticyclones, Desert Climates, Dew point, Harmful effects of atmospheric pollution, Elevation precipitations, Energy losses, Equatorial and Tropical Climates, Equatorial weather disturbances, Air mass source regions and frontal zones as a basis of classification, Cold and warm fronts, Frost, Global circulation systems, Global radiation, Highland climate, Homosphere & Troposphere, Humid Climates Temperature, Humid Climates, Humidity, Hygrometers, Icebergs, Icecap climate, Insolation, Pollution inversion, Jet stream, The Koppen climate classification system, The Koppen climate classification system (2), Land and water differences, Latent Heat, Latitude, Littoral Climates, Local winds, Marine Climates, Air masses classification, Mediterranean Climates, Middle Climates, Monsoon winds, North American Air masses, Northern pressure, Open System, Orographic & Cyclonic Precipitations, Phenomena of the outer atmosphere, Permafrost, Polar, Arctic, and Highland Climates, Pollution sources, Precipitation as a basis for climate classification, Precipitation conditions, Precipitation measure, Precipitations, Radiation balance, Rainforest Climates, Sea ice, Smog, Soil moisture as a basis for climate classification, Steppe Climates, Steppes Climates, Marine sub arctic climate, Subtropical Climates, Surface pressure, Thornthwaite's Climates Classification, Thornthwaite's Climates Classification (2), Thunderstorms, Tornadoes, Traveling cyclones, Trewartha's Climates Classification, Trewartha's Climates Classification (2), Trewartha's Climates Classification (3), Tropical Cyclones, Tropical Cyclones Distribution, Troposphere & Man, Tundra climate, Urbanisation, Vegetation and Climate, Wave cyclones, Weather Control, West Climates, Wet-Dry Climates, Wind systems, Winds,
Atmospheric moisture

Moisture

Plant and animal life of the lands, upon which man depends for much of his food, require fresh water. Man himself uses fresh water in many ways. The only basic source of fresh water is from the atmosphere through condensation of water vapour.

Water also leaves the land and ocean surfaces by evaporation and so returns to the atmosphere. Evidently, the global pathways of movement of water form a complex network. We have already mentioned that there is a global water balance, just as there is an energy balance, and that the water balance deals with flow of matter and so compliments the energy balance.


Water states and heat - Water occurs in three states,

  • (1) frozen as ice, a crystalline solid,,
  • (2) liquid as water, and
  • (3) gaseous as water vapour.

    From the gaseous vapour state, molecules may pass into the liquid state by condensation, or if temperatures are below the freezing point, they can pass by sublimation directly into the solid state to form ice crystals. By evaporation, molecules can leave a water surface to become gas molecules in water vapour. The analogous change from ice directly into water vapour is also designated sublimation. Then, of course, water may pass from liquid to solid state by freezing, and from solid state to liquid state by melting. All of this can be represented by a triangle in which the three states of water form the comers. Arrows show the six possible changes of state.

    Of great importance in weather science are the exchanges of heat energy accompanying changes of state. For example, when water evaporates, sensible heat, which we can feel and measure by thermometer, passes into a hidden form held by the water vapour and known as the latent heat of vaporization. This results, in a drop in temperature of the remaining liquid, the cooling effect produced by evaporation of perspiration from the skin is perhaps the most obvious example. For every gram of water that is evaporated, about 600 calories change into the latent form. In the reverse process of condensation, an equal amount of energy is released to become sensible heat and the temperature rises correspondingly. Similarly, the freezing process releases heat energy in the amount of about 80 calories per gram of water, whereas melting absorbs an equal quantity of heat. This is referred to as the latent heat of fusion. When sublimation occurs, the heat absorbed by vaporization, or released by crystallization, is still greater for each gram of water, for the latent heats of vaporization and fusion are added together.

    Next: Biochemical Cycle


  • "The world is a book, and those who do not travel read only a page", St. Augustine said. Here at www.travel-university.org we believe that every page must be read and explored. Travel is an avenue of learning that no text or classroom can teach. The world is a living classroom and you the student. We invite you to the www.travel-university.org library where you can read general interest and detail oriented articles.





    Google


    this site
    Web

    Your travel reference

    © www.travel-university.org 2004-2010 - All materials contained in this website are protected by c o p y r i g h t laws, and may not be reproduced, republished, distributed, transmitted, displayed, broadcast or otherwise exploited in any manner without the express prior written permission of www.travel-university.org. You may link from your website to www.travel-university.org homepage or one of its interior pages. We do not run a links exchange program per se, but you may contribute by writing about a travel article that includes a link to your website in its text; see guidelines in our Contributors page.
    Contact us