Mainly sources with climatic data, summarized over a period, were selected for the bibliography. In addition, the years from 1940 to the termination date (April 15, 1960) were emphasized in choosing sources. The initials DWB, DLC and DN-HO used in the abstract titles refer to the Weather Bureau Library, the Library of Congress and the U.S. Navy Hydrographic Office Library all in Washington, D.C. Preparation of these abstracts was done in the Foreign Area Section of the Office of Climatology. All scales with brackets are measured with a natural map scale indicator from maps with latitude lines and are only an estimation. Those scales without brackets in the abstracts are given on the climatic maps or a legend scale provided. On maps without parallels, latitude lines were estimated and a natural map scale used to obtain an approximate map scale; these are indicated by parenthesis. (Author).

The Physical Oceanography of the Arctic Mediterranean Sea describes the circulation and the processes in the Arctic Mediterranean, how our present knowledge has developed, and presents recent changes caused by a gradually warmer global climate.The Arctic Mediterranean Sea has been intensively studied in recent years, especially during the fourth International Polar Year, 2007–09, and we have become increasingly aware of the changes presently taking place. This book collects and presents newly acquired knowledge and sets it in perspective to previous studies. Authored by a world-renowned leader in the field, this book explores the role of this small but important sea in the global oceanic circulation and climate—a must-read for researchers and students in the fields of oceanography and climate science. - Relates observed features to active processes and provides sufficient background information to understand the theoretical explanations - Presents the Arctic Mediterranean Sea in the context of global ocean circulation and climate - Presents a modern, comprehensive, and coherent treatment of Arctic (and subarctic) physical oceanography

Gisela Kutzbach has provided an unparalleled account of the mainstream of meteorological thought during the nineteenth and early twentieth centuries. This book takes us from the era of attempts to describe disturbances as mechanistic interactions of air currents, through Espy's introduction in the 1830's of the proposition that cyclones are convective systems driven by heat of condensation in central rainy areas, up to the distinctively different polar front theory of 1920, often considered as the birth of modern meteorology. Follies and controversies as well as successes are recounted, and in the tale the cast of characters, many of them acute observers or experimenters as well as theoreticians, and some crusty and dogmatic, are brought to life. The period was one in which basic concepts of thermodynamics, hydrodynamics, and energy conversions emerged with parallel accommodations to the special needs of meteorology. Influences of the development of synoptic meteorology and early aerology are thoroughly treated, essential mathematical expositions are presented in their original forms with explications, and theories and analyses are illuminated by numerous well-chosen figures and quotations. Concise but complete, and written in a style easy to comprehend, the treatise is a lively account of a lively time in the development of science. Kutzbach has succeeded well in her objectives, to provide "an insight in the particular problems and methods of problem solving in nineteenth century meteorology" and to illustrate "that science is a human activity and that its development is an open-ended process involving the constant testing of hypotheses."