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...
Main Authors: | , , , , |
---|---|
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 |
id |
doaj-cec3e35db74440af86e556756c540430 |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT cpdavis 3dpolarisedsimulationsofspacebornepassivemmsubmmmidlatitudecirrusobservationsacasestudy AT kfevans 3dpolarisedsimulationsofspacebornepassivemmsubmmmidlatitudecirrusobservationsacasestudy AT sabuehler 3dpolarisedsimulationsofspacebornepassivemmsubmmmidlatitudecirrusobservationsacasestudy AT dlwu 3dpolarisedsimulationsofspacebornepassivemmsubmmmidlatitudecirrusobservationsacasestudy AT hcpumphrey 3dpolarisedsimulationsofspacebornepassivemmsubmmmidlatitudecirrusobservationsacasestudy |
_version_ |
1725508858354335744 |