Measuring Radiation Balance at Sea PDF Download
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Author: N. E. Ter-Markari͡ant͡s
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 486
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Book Description
Author: N. E. Ter-Markari͡ant͡s
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 486
Get Book Here
Book Description
Author: N. E. Ter-Markari︠a︡nt︠s︡
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 0
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Book Description
![Measuring Radiation Balance at Sea [with List of References] PDF](https://books.google.com/books/content/images/frontcover/dal1tAEACAAJ?fife=w80-h100)
Author:
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 20
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Book Description
Author: Alex M. Sturrock
Publisher:
ISBN:
Category : Atmospheric radiation
Languages : en
Pages : 36
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Book Description
Author: Ehrhard Raschke
Publisher: Springer Science & Business Media
ISBN: 3662032899
Category : Science
Languages : en
Pages : 611
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Book Description
The study of the earth's climate requires reliable global data sets to validate numerical simulation models and to identify regional and global fluctuations and trends. This book presents ways to obtain such data from space-borne and ground-based measurements, both passive and active, over the entire electromagnetic spectrum. It describes the basics of such methods together with the most recent advancements and spans the field from clouds and the planetary radiation budget to surface processes and ocean properties. Each subject is backed by extensive reference lists to enable readers to probe more deeply.
Author: David Raymond Minard
Publisher:
ISBN:
Category : Solar radiation
Languages : en
Pages : 148
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Book Description
Solar radiation intensities, incident to the sea surface off the Oregon coast, are measured and compared. Simplification of some physical and biological problems can be anticipated if the average radiation received over a broad segment of ocean can be accurately indicated by the amount recorded at the land station. The area of ocean over which the study was made extends the length of the Oregon coast and 165 miles to sea. The measurements were made during the months of June, July, August, and September 1963 with an Eppley total radiation pyrheliometer. A division of the study area into Newport and three zones parallel to the coast separated the data into comparative groups. Clear sky radiation values, assumed constant with longitude, are used as bases for comparison. For each value of observed radiation, a corresponding clear sky value was calculated using standard techniques. Curves, based on a dust-free atmosphere with two cm of precipitable water, are developed to provide these calculated values. Before the recorded values from the zones are compared, their corresponding calculated spectra are adjusted to be identical. This is done by weighting the number of observations in each classification. In all instances, the zone values are adjusted to those of Newport. Comparison is made between mean intensity values, percentages of calculated clear sky values, relative and cumulative frequencies of intensities, and composites of daily traces. Two methods of analysis are employed. One classifies data by intensity level, and the other classifies it by the hour of the day during which it was recorded. Not enough observations were available in the two zones farthest from Newport to provide smooth curves. It is found, however, that there is essentially no change with longitude in observed intensity spectra and means. It is concluded that the average radiation recorded at Newport indicates with some accuracy the average radiation received over the section of ocean in question.
Author: John Monteith
Publisher: Butterworth-Heinemann
ISBN: 9780713129311
Category : Nature
Languages : en
Pages : 308
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Book Description
Thoroughly revised and up-dated edition of a highly successful textbook.
Author: V. S. Samoilenko
Publisher:
ISBN:
Category :
Languages : en
Pages : 47
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Book Description
It is the purpose of the present paper to familiarize the reader with certain results of experimental measurements of the radiation balance and atmospheric emission at various altitudes above sea level, these measurements having been carried out in the Black Sea in 1961 and 1962. These measurements were undertaken to verify preliminary theoretical calculations based on the prevailing scientific conceptions of the emittance and absorptance of the basic substances within the composition of atmospheric air above seas and oceans. With regard to water vapor, this test was extremely necessary, since the contentions on which the calculations of the balance of the longwave infrared emission of the earth and of the atmosphere are based have been taken up to the present time primarily from laboratory rather than from natural studies. However, the natural investigations of these water-vapor absorption spectra in the region of atmospheric emission are carried out extremely infrequently because of the complexity involved. It is for this reason that the numerical values of the absorption coefficients derived from the laboratory studies are not sufficiently accurate. (Author).
Author: Ian S. Robinson
Publisher: Springer Science & Business Media
ISBN: 9783540426479
Category : Science
Languages : en
Pages : 752
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Book Description
This book covers the fundamental principles of measuring oceans from space, and also contains state-of-the-art developments in data analysis and interpretation and in sensors. Completely new will be material covering advances in oceanography that have grown out of remote sensing, including some of the global applications of the data. The variety of applications of remotely sensed data to ocean science has grown significantly and new areas of science are emerging to exploit the gobal datasets being recovered by satellites, particularly in relation to climate and climate change, basin-scale, air-sea interaction processes (e.g. El Nino) and the modelling, forecasting and prediction of the ocean.
Author: K. N. Liou
Publisher: Academic Press
ISBN: 0124514510
Category : Nature
Languages : en
Pages : 599
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Book Description
Fundamentals of radiation for atmospheric applications -- Solar radiation at the top of the atmosphere -- Absorption and scattering of solar radiation in the atmosphere -- Thermal infrared radiation transfer in the atmosphere -- Light scattering by atmospheric particulates -- Principles of radiative transfer in planetary atmospheres -- Application of radiative transfer principles to remote sensing -- Radiation and climate.
