by Naval Postgraduate School, Available from National Technical Information Service in Monterey, Calif, Springfield, Va .
Written in English
This is the final report of the study on the winter atmospheric circulation for the decade 1974-1983. Part I is an observational study of the time mean flow and transients for the northern wintertime for the period 1974/5 to 1982/3. Part II is an observational study of the divergent flow for the tropics and midlatitudes in the northern wintertime for the period 1974/5 to 1982/3. Keywords: Jet streams; Winter storms; Global geographical distributions; Synoptic meteorology; Transient kinetic energy fields; Eddies(Fluid mechanics); Vortices; Northern hemisphere.
|Statement||James S. Boyle, C.-P. Chang|
|Contributions||Chang C.-P. (Chih-Pei), Naval Postgraduate School (U.S.). Dept. of Meteorology|
|The Physical Object|
|Pagination||vi, 79 p. :|
|Number of Pages||79|
Murry Salby's new book provides an integrated treatment of the processes controlling the Earth-atmosphere system, developed from first principles through a balance of theory and applications. This book builds on Salby's previous book, Fundamentals of Atmospheric :// The PMEL website has been updated, and many URLs have changed. To find your page Please use the navigation at the top of this page or the sitemap or the "Search PMEL Home" box in the upper right corner of the page Please update your links. If you followed a link, please contact the originating site's webmaster with a request that they update their :// 2 days ago The Artist’s Reserved Rights Transfer and Sale Agreement (Siegelaub-Projansky Agreement) of and the certificates of early Conceptual art have been considered contradictory for enabling so-called “dematerialized” artworks to be exchanged as any other commodifiable work, thus negating Conceptual artists’ claims of challenging market and institutional :// Chapter 5 Extratropical Planetary-Scale Circulations Introduction This chapter will discuss observational and theoretical aspects of some of the planetary-scale "climatological" features of the extratropical stratosphere and mesosphere, which vary slowly from month to month during the annual cycle and recur regularly from year to ://
4 See for example Steve Bruce, The Red Hand: Protestant Paramilitaries in Northern Ireland (Oxford: Oxford University Press ). 5 A fairly accurate first hand account of this period is presented in Sean MacStiofain, Revolutionary In Ireland (Great Britain: Saxon House ) pp– No one knows for sure. In the Devils Hole, Nevada, paleoclimate record, the last four interglacials lasted over ~20, years with the warmest portion being a relatively stable period of 10, to 15, years duration. This is consistent with what is seen in the Vostok ice core from Antarctica and several records of sea level high :// Last winter, we saw that in a smaller scale here in the UK. Most records came from London at the time, and so widespread detail wasnt available. If it was, I think rural locations in Central and Northern parts, may have seen very cold minimums and maximums, possible into the The main threat to British democracy in the s arose from the activities of the political right and the security services. Unaccountable elements in the security services and military intelligence created covert operations such as ‘Clockwork Orange’, which smeared left wing figures in Northern Ireland and Britain, as well as providing Protestant paramilitaries with the names and
First copyright renewals for periodicals This is an inventory of periodicals and their first copyright renewals (if any). Most periodicals published in the US prior to had to renew their issue copyrights after 28 years in order to retain copyright on the :// Based on daily reports from the global radiosonde network for the yr period from to , Oort () estimated and as − and W m −2, respectively, revealing the dominant role of relative to , and concluded that the indirect Ferrel circulation consumes zonal mean kinetic energy at a rate slightly exceeding production by The Red Sea hosts a deep marine environment unique among the world’s oceans. It is occupied, almost homogeneously from the subsurface (~ to m) to depths over m, by a warm (~°C) and highly saline (~) water mass, referred to as the Red Sea Deep Water (RSDW). Previous studies suggested that the RSDW is mainly ventilated, continuously or intermittently, by dense outflows The latter also prevents a good view of South Pacific high subsidence except in the northern winter. The cross sections, however, clearly show the complex vertical structure of the deep-tropospheric circulation combined with the shallow overturning below mb in both hemispheres. In January, ω at mb does not indicate the main activity at