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  • Iselin, Columbus O’Donnell (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1936-08)
    With the opening of the Woods Hole Oceanographic Institution in July 1931, there was inaugurated a program of investigations in the deep waters of the western North Atlantic for which there had long been a great need. ...
  • Seiwell, Harry Richard (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1937-05)
    With the advance in knowledge of oceanic circulation there now exists a demand for additional identifying properties which will serve to trace the origin and movements of water masses in the sea, and to check earlier ...
  • Seiwell, Harry Richard (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1937-05)
    Because of general interest in the subject of vertical oscillations in the sea and because such information is scanty for the ocean basins, an investigation of the question in the western North Atlantic was initiated by ...
  • Stetson, Henry C. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-07)
    Our knowledge of clastic, shallow-water sediments over any considerable area of ocean floor is very generalized and leaves much to be desired. The notations concerning the character of the bottom found on all charts are ...
  • Montgomery, Raymond B. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-08)
    Except for the presence in most localities of a shallow homogeneous surface layer and of a relatively homogeneous and deeper bottom layer, the oceans of the temperate and tropical regions are stratified and vertically ...
  • Seiwell, Harry Richard (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-09)
    Observational data for this discussion were obtained principally during the two cruises of the oceanographic research ship, "Atlantis," to the Caribbean Sea March 7 to May 5, 1933 (stations 1487-1610) and February 2 to ...
  • Houghton, Henry G.; Radford, W. H. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-10)
    It is submitted that the hazards of landing aircraft in fog could be greatly reduced by providing relatively small clearings into which approaching planes could be safely guided by radio or other navigational aids which ...
  • Houghton, Henry G.; Radford, W. H. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-11)
    A short critical review of possible methods for the measurement of the size of fog particles is presented. It is concluded that the only suitable method of obtaining the distribution of drop sizes present in a given fog ...
  • Rossby, Carl-Gustaf; Namias, Jerome; Simmers, Ritchie G. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1938-12)
    This paper constitutes Part I of a report on certain investigations which have been in progress at the Massachusetts Institute of Technology during the past few years and which have been supported in part with funds ...
  • Avsec, Dusan (E. Blondel la Rougery : Gauthier-VillarsWoods Hole Oceanographic Institution, 1939)
    The object of the present work is a study thermoconvective eddies in a layer of air heated uniformly from below. Being given the importance that these eddies present in meteorlogical phenomena, we have tried to attain three ...
  • Seiwell, Harry Richard (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1939-11)
    This paper is a discussion of possible discrepancies in computations of ocean currents (based on horizontal variations of dynamic topography calculated from arbitrary deep lying reference surfaces), because of time ...
  • Montgomery, Raymond B. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1940-02)
    In order to obtain information on the effect of eddy viscosity and eddy diffusion at the boundary between sea and atmosphere, simultaneous measurements of humidity at two, three or four levels between 1 and 38 meters ...
  • Allen, R. A.; Fletcher, R.; Holmboe, J.; Namias, Jerome; Willett, Hurd C. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1940-04)
    The following report is presented as a statement of progress made at the Massachusetts Institute of Technology (M.I.T.) in the investigation into the possibility of extending the range of reliable weather forecasts. This ...
  • Iselin, Columbus O’Donnell (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1940-07)
    In 1937 the Woods Hole Oceanographic Institution and the Bermuda Biological Station for Research agreed to cooperate on a five year program of observations. This was designed to throw light on the general problem of ...
  • Garstens, M. A. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1941-04)
    In recent years great interest has developed in the study of the role of the semipermanent centers of action as they affect weather conditions averaged over several days. An examination of the daily synoptic and upper ...
  • Brooks, Frederick A, (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1941-10)
    Atmospheric radiation is the primary variable in nocturnal cooling, although wind has greater influence on the temperature of surface air. Since temperature inversions near the ground cannot be formed unless surfaces are ...
  • Willett, Hurd C.; Allen, R. A.; Namias, Jerome (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1941-11)
    The present report is intended to cover fully the activities of the long-range forecast project both at the Massachusetts Institute of Technology and at the U. S. Weather Bureau in Washington, between July 1, 1940, and ...
  • Petterssen, Sverre; Austin, James Murdoch (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1942-01)
    Soon after the discovery of the polar front, it was realized that fronts were subject to processes which either increased or diminished their intensity. Thus, fronts may form in fields where the distributiori of the ...
  • Iselin, Columbus O’Donnell; Woodcock, A. H. (Woods Hole Oceanographic Institution, 1942-07-25)
    With moderate or light winds and a clear sky the diurnal heating which occurs near the sea surface can cause a serious reduction in the range of submarine detection, especially on shallow targets. This has usually been ...
  • Redfield, Alfred C. (Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1942-09)
    The great oceans of the world all contain at intermediate depths less oxygen and more nitrate and phosphate than is found at either lesser or greater depths. This is one of the most marked physical features of the sea ...

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