Phase Arctic Cloud Experiment (M-PACE).
The importance of arctic cloud properties to the surface radiative flux budget is well known, and accurate representation of these clouds is essential to proper modeling of the arctic environment. One of the interesting characteristics of arctic clouds is the prevalence of mixed phase cloud layers....
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.176.3628 2023-05-15T14:38:13+02:00 Phase Arctic Cloud Experiment (M-PACE). M. Poellot D. Brown The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.176.3628 http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.176.3628 http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf text ftciteseerx 2016-01-07T16:15:00Z The importance of arctic cloud properties to the surface radiative flux budget is well known, and accurate representation of these clouds is essential to proper modeling of the arctic environment. One of the interesting characteristics of arctic clouds is the prevalence of mixed phase cloud layers. In these mixed-phase clouds, the water content tends to dominate the radiative effects, causing them to act as all liquid clouds. Measurements have shown these clouds to be highly inhomogeneous in terms of ice and liquid water content. The horizontal dimension is important to proper interpretation of remotely sensed data where properties are averaged over space and/or time. It is also of interest to the modeling community for the parameterization of sub-grid scale features. The objective of this research is to characterize the horizontal variability of the cloud microphysical properties sampled during the Mixed- Text Arctic Unknown Arctic |
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English |
description |
The importance of arctic cloud properties to the surface radiative flux budget is well known, and accurate representation of these clouds is essential to proper modeling of the arctic environment. One of the interesting characteristics of arctic clouds is the prevalence of mixed phase cloud layers. In these mixed-phase clouds, the water content tends to dominate the radiative effects, causing them to act as all liquid clouds. Measurements have shown these clouds to be highly inhomogeneous in terms of ice and liquid water content. The horizontal dimension is important to proper interpretation of remotely sensed data where properties are averaged over space and/or time. It is also of interest to the modeling community for the parameterization of sub-grid scale features. The objective of this research is to characterize the horizontal variability of the cloud microphysical properties sampled during the Mixed- |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
M. Poellot D. Brown |
spellingShingle |
M. Poellot D. Brown Phase Arctic Cloud Experiment (M-PACE). |
author_facet |
M. Poellot D. Brown |
author_sort |
M. Poellot |
title |
Phase Arctic Cloud Experiment (M-PACE). |
title_short |
Phase Arctic Cloud Experiment (M-PACE). |
title_full |
Phase Arctic Cloud Experiment (M-PACE). |
title_fullStr |
Phase Arctic Cloud Experiment (M-PACE). |
title_full_unstemmed |
Phase Arctic Cloud Experiment (M-PACE). |
title_sort |
phase arctic cloud experiment (m-pace). |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.176.3628 http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic |
genre_facet |
Arctic |
op_source |
http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.176.3628 http://www.arm.gov/publications/proceedings/conf16/extended_abs/poellot_m.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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