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contributor authorStolov, Harold L.
contributor authorSpar, Jerome
date accessioned2017-06-09T14:14:18Z
date available2017-06-09T14:14:18Z
date copyright1968/01/01
date issued1968
identifier issn0022-4928
identifier otherams-15394.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4151061
description abstractSurface atmospheric pressures are studied for periods before and after chromospheric flares by the superposed epoch method for 31 meteorological stations in North America. The individual analyses show no statistically significant pressure departures following the flares. No evidence is found for claims that continental and coastal stations exhibit different responses to the flares. No evidence is found for claims that atmospheric pressure responses to flares are amplified with increasing latitude. The composite curve for North American stations shows no statistically significant departures and does not verify the composite curve of previous investigators. Chromospheric flares with polar cap absorption (PCA) events and chromospheric flares without PCA events are indistinguishable in the response of surface atmospheric pressure in the polar cap, failing to support the claims of previous investigators. All the departures observed in this study of North American data can be explained by the ordinary transient meteorological variations of the pressure field.
publisherAmerican Meteorological Society
titleSearch for Tropospheric Responses to Chromospheric Flares
typeJournal Paper
journal volume25
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1968)025<0126:SFTRTC>2.0.CO;2
journal fristpage126
journal lastpage132
treeJournal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 001
contenttypeFulltext


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