Tucson / New York / Oxford / Washington / DC / Cambridge / Livermore / London / Bremen / /
Company
R. W. Murray L. C. / Amazon / R. B. Pearce L. C. / Lawrence Livermore National Laboratory / J. T. Overpeck L. C. / L. Lin L. C. / C. O’Hara L. C. / /
Continent
South America / /
Country
Switzerland / Germany / Greenland / Venezuela / Netherlands / Pakistan / United States / Brazil / Panama / China / /
Currency
pence / / /
Event
Environmental Issue / /
Facility
University of Miami / Swiss Federal Institute of Technology / University of Arizona / University of Bremen / the Netherlands Institute / University of Colorado / /
IndustryTerm
greenhouse gas / deep energy source / convection solutions / chemical elemental composition / /
NaturalFeature
Atlantic Ocean / Andes / North Atlantic sea / Orinoco / Pacific Ocean / Venezuelan coast / /
Organization
Division of Ocean Sciences / Swiss Federal Institute of Technology / National Science Foundation / Department of Earth Sciences / Woods Hole Oceanographic Institution / Department of Marine Chemistry and Geochemistry / Cambridge Univ. / Department of Geosciences / University of Miami / Miami / American Geophysical Union / Rosenstiel School of Marine and Atmospheric Science / University of Colorado / Boulder / University of Bremen / Institute for Sea Research / National Aeronautics and Space Administration / Particle Physics and Astronomy Research Council / University of Arizona / Department of Geological Sciences / Oceanographic Institution / /
Person
Woods Hole / /
ProvinceOrState
New York / Florida / California / Arizona / Massachusetts / Colorado / /
Region
northern Venezuela / North Atlantic / northeastern Brazil / western North Atlantic / eastern Caribbean / Caribbean / southern Caribbean / northern South America / /
REPORTS tration for Ta ⫽ 10 when ␦ ⱖ O(10). In the case of the jovian atmosphere, if we take Ta ⫽ 1012 for Jupiter (9), we obtain ␦ ⫽ 100. Teleconvection may have important implications for the dynamics of pl