3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study

Global observations of ice clouds are needed to improve our understanding of their impact on earth's radiation balance and the water-cycle. Passive mm/sub-mm has some advantages compared to other space-borne cloud-ice remote sensing techniques. The physics of scattering makes forward radiat...

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Main Authors: C. P. Davis, K. F. Evans, S. A. Buehler, D. L. Wu, H. C. Pumphrey
Format: Article
Language:English
Published: Copernicus Publications 2007-08-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/7/4149/2007/acp-7-4149-2007.pdf
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spelling doaj-cec3e35db74440af86e556756c5404302020-11-24T23:40:52ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242007-08-01715414941583-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case studyC. P. DavisK. F. EvansS. A. BuehlerD. L. WuH. C. PumphreyGlobal observations of ice clouds are needed to improve our understanding of their impact on earth's radiation balance and the water-cycle. Passive mm/sub-mm has some advantages compared to other space-borne cloud-ice remote sensing techniques. The physics of scattering makes forward radiative transfer modelling for such instruments challenging. This paper demonstrates the ability of a recently developed RT code, ARTS-MC, to accurately simulate observations of this type for a variety of viewing geometries corresponding to operational (AMSU-B, EOS-MLS) and proposed (CIWSIR) instruments. ARTS-MC employs an adjoint Monte-Carlo method, makes proper account of polarisation, and uses 3-D spherical geometry. The actual field of view characteristics for each instrument are also accounted for. A 3-D midlatitude cirrus scenario is used, which is derived from Chilbolton cloud radar data and a stochastic method for generating 3-D ice water content fields. These demonstration simulations clearly demonstrate the beamfilling effect, significant polarisation effects for non-spherical particles, and also a beamfilling effect with regard to polarisation. http://www.atmos-chem-phys.net/7/4149/2007/acp-7-4149-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C. P. Davis
K. F. Evans
S. A. Buehler
D. L. Wu
H. C. Pumphrey
spellingShingle C. P. Davis
K. F. Evans
S. A. Buehler
D. L. Wu
H. C. Pumphrey
3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
Atmospheric Chemistry and Physics
author_facet C. P. Davis
K. F. Evans
S. A. Buehler
D. L. Wu
H. C. Pumphrey
author_sort C. P. Davis
title 3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
title_short 3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
title_full 3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
title_fullStr 3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
title_full_unstemmed 3-D polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
title_sort 3-d polarised simulations of space-borne passive mm/sub-mm midlatitude cirrus observations: a case study
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2007-08-01
description Global observations of ice clouds are needed to improve our understanding of their impact on earth's radiation balance and the water-cycle. Passive mm/sub-mm has some advantages compared to other space-borne cloud-ice remote sensing techniques. The physics of scattering makes forward radiative transfer modelling for such instruments challenging. This paper demonstrates the ability of a recently developed RT code, ARTS-MC, to accurately simulate observations of this type for a variety of viewing geometries corresponding to operational (AMSU-B, EOS-MLS) and proposed (CIWSIR) instruments. ARTS-MC employs an adjoint Monte-Carlo method, makes proper account of polarisation, and uses 3-D spherical geometry. The actual field of view characteristics for each instrument are also accounted for. A 3-D midlatitude cirrus scenario is used, which is derived from Chilbolton cloud radar data and a stochastic method for generating 3-D ice water content fields. These demonstration simulations clearly demonstrate the beamfilling effect, significant polarisation effects for non-spherical particles, and also a beamfilling effect with regard to polarisation.
url http://www.atmos-chem-phys.net/7/4149/2007/acp-7-4149-2007.pdf
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