Remote Sensing and Atmospheric Ozone
Remote Sensing and Atmospheric Ozone

Author: Arthur Philip Cracknell

Publisher: Springer Science & Business Media

Published: 2012-06-21

Total Pages: 701

ISBN-13: 3642103340

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The destruction of the ozone layer, together with global warming, is one of the hot environmental topics of today. This book examines the effect of human activities on atmospheric ozone, namely the increase of tropospheric ozone and the general diminution of stratospheric ozone and the production of the Antarctic ozone hole. Also discussed is the role of remote sensing techniques in the understanding of the effects of human activities on atmospheric ozone as well as in the development of social and political awareness of the damage to the ozone layer by man-made chemicals, principally CFCs. This led to the formulation and ratification in 1989 of the Montreal Protocol on controlling/banning the manufacture and use of chemicals that damage the ozone layer. Since then, remote sensing has played a key role in monitoring atmospheric ozone concentration and determining the success of the Montreal Protocol in protecting the ozone layer from further damage. In this book, the renowned authors discuss the sophisticated instruments that have been launched into space to study not only ozone but also other trace gases in the atmosphere, some of which play a key role in the generation and destruction of ozone in the atmosphere. Professors Cracknell and Varotsos also examine the satellite-flown instruments which are involved in monitoring the absorption of solar ultraviolet light in the atmosphere in relation both to the generation and destruction of ozone and consequently to human health. This scholarly book, written by the foremost experts in the field, looks at remote sensing and its employment in the various aspects of ozone science. It is widely acknowledged that global warming, due to anthropogenic greenhouse gases emissions, represents a threat to the sustainability of human life on Earth. However, many other threats are potentially just as serious, including atmospheric pollution, ozone depletion, water pollution, the degradation of agricultural land, deforestation, the depletion of the world's mineral resources and population growth.

Atmospheric Ultraviolet Remote Sensing
Atmospheric Ultraviolet Remote Sensing

Author: Robert E. Huffman

Publisher: Academic Press

Published: 1992-10-19

Total Pages: 331

ISBN-13: 0080918808

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This book is an introduction to the use of the ultraviolet for remote sensing of the Earth's atmosphere. It covers the Earth's UV radiative environment, experimental techniques, and current applications. it is my intention to provide the information needed to "make a first approximation" concerning the use of the ultraviolet and to provide access through the literature for a more thorough study. * Contains recent UV applications not previously available in book form such as ozone, auroral images, and ionospheric sensing * Features broad coverage of fundamentals of atmospheric geophysics with values for fluxes, cross-sections, and radiances * Covers techniques that illustrate principles of measurements with typical values * Contains numerous references to original literature

Seasonal and Geographic Variation of Atmospheric Ozone, Derived from Nimbus 3
Seasonal and Geographic Variation of Atmospheric Ozone, Derived from Nimbus 3

Author: C. Prabhakara

Publisher:

Published: 1971

Total Pages: 76

ISBN-13:

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Nimbus 3 infrared interferometer spectrometer (IRIS)measurements of the intensities in the 9.6-pn region are used to derive the ozone content in the atmosphere between latitudes SOON and 80's. The global distribution of total ozone was mapped for eight days in April and eight days in July 1969. These global maps of total ozone are compared with the upper-air oonstant pressure maps to emphasize the meteorological significance of the ozone variations in time and space. The total ozone has a minimum value of about 0.25 cm STP in the equatorial regions and increases markedly toward both poles. In the Arctic region, the total ozone in the spring time is well above 0.5 cm STP, while in summer it is about 0.4 cm STP. An eight-day mean global map of total ozone for April 1969 clearly reveals the presence of climatological large-scale ozone systems in the atmosphere. Another such map, for July 1969, shows that these systems have weakened considerably in the northern hemisphere. Seasonal variability in the total ozone over the southern hemisphere is much less pronounced. Close association between the total-ozone systems and tropospheric weather systems is shown for several cases. From this study, it is concluded that the atmospheric ozone, remotely sensed by satellites, can be used as a meteorological parameter to diagnose the present state of the atmosphere, and, thereby, aid weather prediction.