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    VISIBILITY AND LIQUID WATER CONTENT IN CLOUDS IN THE FREE ATMOSPHERE 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 001:;page 54
    Author(s): aufm Kampe, H. J.
    Publisher: American Meteorological Society
    Abstract: Koschmieder's formula is verified by experimental data obtained on Mt. Washington and is used to determine visibility in clouds from measurements of the scattering coefficient. Visibility in clouds varies from approximately ...
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    VISIBILITY AND LIQUID WATER CONTENT IN THE FREE ATMOSPHERE 

    Source: Journal of Meteorology:;1950:;volume( 007 ):;issue: 002:;page 166
    Author(s): aufm Kampe, H. J.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    UPPER-AIR WIND MEASUREMENTS WITH SMALL ROCKETS 

    Source: Journal of Meteorology:;1956:;volume( 013 ):;issue: 006:;page 601
    Author(s): aufm Kampe, H. J.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    THE EFFECTIVENESS OF NATURAL AND ARTIFICIAL AEROSOLS AS FREEZING NUCLEI 

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 005:;page 283
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: Measurements of the effectiveness of natural and artificial freezing-nuclei were carried out in a room-size cold chamber. The concentration of natural nuclei varied from approximately one per liter at about ?13C to 1000 ...
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    REPLY 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 005:;page 402
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    PHYSICAL PROPERTIES OF CUMULUS CLOUDS 

    Source: Journal of Meteorology:;1953:;volume( 010 ):;issue: 003:;page 204
    Author(s): Weickmann, H. K.; aufm Kampe, H. J.
    Publisher: American Meteorological Society
    Abstract: Measurements of droplet size and visibility have been made at different levels above the base of all types of cumulus clouds. The evaluation of these data permits calculations of corresponding values of water content and ...
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    REPLY 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 001:;page 81
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    REPLY 

    Source: Journal of Meteorology:;1954:;volume( 011 ):;issue: 005:;page 429
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    ADDITIONAL COMMENTS 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 005:;page 376
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: No Abstract Available
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    TRABERT'S FORMULA AND THE DETERMINATION OF THE WATER CONTENT IN CLOUDS 

    Source: Journal of Meteorology:;1952:;volume( 009 ):;issue: 003:;page 167
    Author(s): aufm Kampe, H. J.; Weickmann, H. K.
    Publisher: American Meteorological Society
    Abstract: With use of cloud data collected in all types of cumulus clouds, it is shown that the constant in the Trabert equation is not actually a constant but varies with the character of the droplet spectrum. Trabert's formula ...
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