Characteristics of Type I PSCs Derived from POAM Observations

The characteristics of Polar Ozone and Aerosol Measurement III (POAM 3) observations of Type I Arctic Polar Stratospheric Clouds (PSCs) from 1998 to 2003 are studied using a scheme that discriminates Type la from Ib PSCs. The PSCs observed in these years are studied simultaneously by aligning the da...

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Main Authors: Alfred, Jerome M., Fromm, Michael D., Bokarius, Konstantin, Strawa, Anthony W., Drdla, Katja
Format: Other/Unknown Material
Language:unknown
Published: 2004
Subjects:
Online Access:http://hdl.handle.net/2060/20040081060
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spelling ftnasantrs:oai:casi.ntrs.nasa.gov:20040081060 2023-05-15T15:01:02+02:00 Characteristics of Type I PSCs Derived from POAM Observations Alfred, Jerome M. Fromm, Michael D. Bokarius, Konstantin Strawa, Anthony W. Drdla, Katja Unclassified, Unlimited, Publicly available [2004] application/pdf http://hdl.handle.net/2060/20040081060 unknown Document ID: 20040081060 http://hdl.handle.net/2060/20040081060 Copyright, Distribution as joint owner in the copyright CASI Meteorology and Climatology Quadrennial Ozone Symposium; 3-9 Jun. 2004; Kos; Greece 2004 ftnasantrs 2019-07-21T02:17:35Z The characteristics of Polar Ozone and Aerosol Measurement III (POAM 3) observations of Type I Arctic Polar Stratospheric Clouds (PSCs) from 1998 to 2003 are studied using a scheme that discriminates Type la from Ib PSCs. The PSCs observed in these years are studied simultaneously by aligning the day in each year when the temperature associated with a POAM observation first reaches T(sub NAT). It is observed that PSC formation occurs within days of the minimum observation temperature reaching T(sub NAT) and that the majority of these first PSCs are Type Ia. Our observations support the hypothesis that heterogeneous freezing contributes at least in part to the freezing of solid phase PSCs. Other/Unknown Material Arctic NASA Technical Reports Server (NTRS) Arctic
institution Open Polar
collection NASA Technical Reports Server (NTRS)
op_collection_id ftnasantrs
language unknown
topic Meteorology and Climatology
spellingShingle Meteorology and Climatology
Alfred, Jerome M.
Fromm, Michael D.
Bokarius, Konstantin
Strawa, Anthony W.
Drdla, Katja
Characteristics of Type I PSCs Derived from POAM Observations
topic_facet Meteorology and Climatology
description The characteristics of Polar Ozone and Aerosol Measurement III (POAM 3) observations of Type I Arctic Polar Stratospheric Clouds (PSCs) from 1998 to 2003 are studied using a scheme that discriminates Type la from Ib PSCs. The PSCs observed in these years are studied simultaneously by aligning the day in each year when the temperature associated with a POAM observation first reaches T(sub NAT). It is observed that PSC formation occurs within days of the minimum observation temperature reaching T(sub NAT) and that the majority of these first PSCs are Type Ia. Our observations support the hypothesis that heterogeneous freezing contributes at least in part to the freezing of solid phase PSCs.
format Other/Unknown Material
author Alfred, Jerome M.
Fromm, Michael D.
Bokarius, Konstantin
Strawa, Anthony W.
Drdla, Katja
author_facet Alfred, Jerome M.
Fromm, Michael D.
Bokarius, Konstantin
Strawa, Anthony W.
Drdla, Katja
author_sort Alfred, Jerome M.
title Characteristics of Type I PSCs Derived from POAM Observations
title_short Characteristics of Type I PSCs Derived from POAM Observations
title_full Characteristics of Type I PSCs Derived from POAM Observations
title_fullStr Characteristics of Type I PSCs Derived from POAM Observations
title_full_unstemmed Characteristics of Type I PSCs Derived from POAM Observations
title_sort characteristics of type i pscs derived from poam observations
publishDate 2004
url http://hdl.handle.net/2060/20040081060
op_coverage Unclassified, Unlimited, Publicly available
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source CASI
op_relation Document ID: 20040081060
http://hdl.handle.net/2060/20040081060
op_rights Copyright, Distribution as joint owner in the copyright
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