Author: N. E. Ter-Markari͡ant͡s
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 486
Book Description
Measuring Radiation Balance at Sea
Author: N. E. Ter-Markari͡ant͡s
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 486
Book Description
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 486
Book Description
Measuring Radiation Balance at Sea
Author: N. E. Ter-Markari︠a︡nt︠s︡
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 0
Book Description
Publisher:
ISBN:
Category : Radiation
Languages : en
Pages : 0
Book Description
Measuring Radiation Balance at Sea [with List of References]
Evaporation and Radiation Measurements at Salton Sea, California
Author: Alex M. Sturrock
Publisher:
ISBN:
Category : Atmospheric radiation
Languages : en
Pages : 36
Book Description
Publisher:
ISBN:
Category : Atmospheric radiation
Languages : en
Pages : 36
Book Description
Radiation and Water in the Climate System
Author: Ehrhard Raschke
Publisher: Springer Science & Business Media
ISBN: 3662032899
Category : Science
Languages : en
Pages : 611
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.
Publisher: Springer Science & Business Media
ISBN: 3662032899
Category : Science
Languages : en
Pages : 611
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.
Solar Radiation Measured at the Sea Surface Off Oregon During Summer 1963
Author: David Raymond Minard
Publisher:
ISBN:
Category : Solar radiation
Languages : en
Pages : 148
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.
Publisher:
ISBN:
Category : Solar radiation
Languages : en
Pages : 148
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.
Principles of Environmental Physics
Author: John Monteith
Publisher: Butterworth-Heinemann
ISBN: 9780713129311
Category : Nature
Languages : en
Pages : 308
Book Description
Thoroughly revised and up-dated edition of a highly successful textbook.
Publisher: Butterworth-Heinemann
ISBN: 9780713129311
Category : Nature
Languages : en
Pages : 308
Book Description
Thoroughly revised and up-dated edition of a highly successful textbook.
An Introduction to Atmospheric Radiation
Author: K. N. Liou
Publisher: Academic Press
ISBN: 0124514510
Category : Nature
Languages : en
Pages : 599
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.
Publisher: Academic Press
ISBN: 0124514510
Category : Nature
Languages : en
Pages : 599
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.
Experimental and Theoretical Investigations of Radiative Heat Exchange in the Surface Layers Above Seas and Oceans
Author: V. S. Samoilenko
Publisher:
ISBN:
Category :
Languages : en
Pages : 47
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).
Publisher:
ISBN:
Category :
Languages : en
Pages : 47
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).
Practical Meteorology
Author: Roland Stull
Publisher: Sundog Publishing, LLC
ISBN: 9780888652836
Category : Science
Languages : en
Pages : 942
Book Description
A quantitative introduction to atmospheric science for students and professionals who want to understand and apply basic meteorological concepts but who are not ready for calculus.
Publisher: Sundog Publishing, LLC
ISBN: 9780888652836
Category : Science
Languages : en
Pages : 942
Book Description
A quantitative introduction to atmospheric science for students and professionals who want to understand and apply basic meteorological concepts but who are not ready for calculus.