Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 /
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....
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ftumichgbhathi:oai:quod.lib.umich.edu:MIU01-011447140 2023-05-15T15:08:00+02:00 Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / Prabhakara, C. Goddard Space Flight Center. United States. National Aeronautics and Space Administration. 1971 bib http://hdl.handle.net/2027/uiug.30112106639864 eng eng Washington, D.C. : National Aeronautics and Space Administration http://hdl.handle.net/2027/uiug.30112106639864 Items in this record are available as Public Domain, Google-digitized. View access and use profile at http://www.hathitrust.org/access_use#pd-google. Please see individual items for rights and use statements. PDM Nimbus (Artificial satellite) Interferometers Ozone Atmospheric ozone text 1971 ftumichgbhathi 2019-11-07T08:06:49Z 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. "N71-32791." Prepared at Goddard Space Flight Center. Includes bibliographical references (p. 47-49). 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. Mode of access: Internet. Text Arctic Hathi Trust Digital Library Arctic |
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Open Polar |
collection |
Hathi Trust Digital Library |
op_collection_id |
ftumichgbhathi |
language |
English |
topic |
Nimbus (Artificial satellite) Interferometers Ozone Atmospheric ozone |
spellingShingle |
Nimbus (Artificial satellite) Interferometers Ozone Atmospheric ozone Prabhakara, C. Goddard Space Flight Center. United States. National Aeronautics and Space Administration. Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
topic_facet |
Nimbus (Artificial satellite) Interferometers Ozone Atmospheric ozone |
description |
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. "N71-32791." Prepared at Goddard Space Flight Center. Includes bibliographical references (p. 47-49). 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. Mode of access: Internet. |
format |
Text |
author |
Prabhakara, C. Goddard Space Flight Center. United States. National Aeronautics and Space Administration. |
author_facet |
Prabhakara, C. Goddard Space Flight Center. United States. National Aeronautics and Space Administration. |
author_sort |
Prabhakara, C. |
title |
Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
title_short |
Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
title_full |
Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
title_fullStr |
Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
title_full_unstemmed |
Seasonal and geographic variation of atmospheric ozone, derived from Nimbus 3 / |
title_sort |
seasonal and geographic variation of atmospheric ozone, derived from nimbus 3 / |
publisher |
Washington, D.C. : National Aeronautics and Space Administration |
publishDate |
1971 |
url |
http://hdl.handle.net/2027/uiug.30112106639864 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_relation |
http://hdl.handle.net/2027/uiug.30112106639864 |
op_rights |
Items in this record are available as Public Domain, Google-digitized. View access and use profile at http://www.hathitrust.org/access_use#pd-google. Please see individual items for rights and use statements. |
op_rightsnorm |
PDM |
_version_ |
1766339434274357248 |