Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*

Antarctic Mesoscale Prediction System (AMPS) forecasts of atmospheric moisture and cloud fraction (CF) are compared with observations at McMurdo and Amundsen–Scott South Pole station (hereafter, South Pole station) in Antarctica. Overall, it is found that the model produces excessive moisture at bot...

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Main Authors: Ryan L. Fogt, David, H. Bromwich
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2006
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.669.3252
http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.669.3252 2023-05-15T13:24:28+02:00 Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS* Ryan L. Fogt David H. Bromwich The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.669.3252 http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.669.3252 http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf text 2006 ftciteseerx 2016-01-08T17:14:52Z Antarctic Mesoscale Prediction System (AMPS) forecasts of atmospheric moisture and cloud fraction (CF) are compared with observations at McMurdo and Amundsen–Scott South Pole station (hereafter, South Pole station) in Antarctica. Overall, it is found that the model produces excessive moisture at both sites in the mid- to upper troposphere because of a weaker vertical decrease of moisture in AMPS than observed. Correlations with observations suggest AMPS does a reasonable job of capturing the low-level moisture variability at McMurdo and the upper-level moisture variability at South Pole station. The model underpredicts the cloud cover at both locations, but changes to the AMPS empirical CF algorithm remove this negative bias by more than doubling the weight given to the cloud ice path. A “pseudosatellite ” product based on the microphysical quantities of cloud ice and cloud liquid water within AMPS is preliminarily evaluated against Defense Meteorological Satellite Program (DMSP) imagery during summer to examine the broader performance of cloud variability in AMPS. These comparisons reveal that the model predicts high-level cloud cover and movement with fidelity, which explains the good agreement between the modified CF algorithm and the observed CF. However, this product also demon-strates deficiencies in capturing low-level cloudiness over cold ice surfaces primarily related to insufficient supercooled liquid water produced by the microphysics scheme, which also reduces the CF correlation with observations. The results suggest that AMPS predicts the overall CF amount and high cloud variability notably well, making it a reliable tool for longer-term climate studies of these fields in Antarctica. 1. Text Amundsen-Scott Antarc* Antarctic Antarctica South pole South pole Unknown Amundsen Scott South Pole Station ENVELOPE(0.000,0.000,-90.000,-90.000) Amundsen-Scott ENVELOPE(0.000,0.000,-90.000,-90.000) Amundsen-Scott South Pole Station ENVELOPE(139.273,139.273,-89.998,-89.998) Antarctic South Pole
institution Open Polar
collection Unknown
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language English
description Antarctic Mesoscale Prediction System (AMPS) forecasts of atmospheric moisture and cloud fraction (CF) are compared with observations at McMurdo and Amundsen–Scott South Pole station (hereafter, South Pole station) in Antarctica. Overall, it is found that the model produces excessive moisture at both sites in the mid- to upper troposphere because of a weaker vertical decrease of moisture in AMPS than observed. Correlations with observations suggest AMPS does a reasonable job of capturing the low-level moisture variability at McMurdo and the upper-level moisture variability at South Pole station. The model underpredicts the cloud cover at both locations, but changes to the AMPS empirical CF algorithm remove this negative bias by more than doubling the weight given to the cloud ice path. A “pseudosatellite ” product based on the microphysical quantities of cloud ice and cloud liquid water within AMPS is preliminarily evaluated against Defense Meteorological Satellite Program (DMSP) imagery during summer to examine the broader performance of cloud variability in AMPS. These comparisons reveal that the model predicts high-level cloud cover and movement with fidelity, which explains the good agreement between the modified CF algorithm and the observed CF. However, this product also demon-strates deficiencies in capturing low-level cloudiness over cold ice surfaces primarily related to insufficient supercooled liquid water produced by the microphysics scheme, which also reduces the CF correlation with observations. The results suggest that AMPS predicts the overall CF amount and high cloud variability notably well, making it a reliable tool for longer-term climate studies of these fields in Antarctica. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ryan L. Fogt
David
H. Bromwich
spellingShingle Ryan L. Fogt
David
H. Bromwich
Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
author_facet Ryan L. Fogt
David
H. Bromwich
author_sort Ryan L. Fogt
title Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
title_short Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
title_full Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
title_fullStr Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
title_full_unstemmed Atmospheric Moisture and Cloud Cover Characteristics Forecast by AMPS*
title_sort atmospheric moisture and cloud cover characteristics forecast by amps*
publishDate 2006
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.669.3252
http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf
long_lat ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(0.000,0.000,-90.000,-90.000)
ENVELOPE(139.273,139.273,-89.998,-89.998)
geographic Amundsen Scott South Pole Station
Amundsen-Scott
Amundsen-Scott South Pole Station
Antarctic
South Pole
geographic_facet Amundsen Scott South Pole Station
Amundsen-Scott
Amundsen-Scott South Pole Station
Antarctic
South Pole
genre Amundsen-Scott
Antarc*
Antarctic
Antarctica
South pole
South pole
genre_facet Amundsen-Scott
Antarc*
Antarctic
Antarctica
South pole
South pole
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http://polarmet.osu.edu/PMG_publications/fogt_bromwich_wf_2008.pdf
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