Some considerations on the infrared cloud forcing

Long-wave spectral cloud forcing is computed for realistic clouds of various optical thickness embedded in the tropical and subarctic winter standard atmospheres. The strict connections between the integrated long-wave cloud forcing (LCF) and cloud's altitude and transmissivity are shown. LCF,...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Rizzi R., Maestri T.
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:https://hdl.handle.net/11585/956459
https://doi.org/10.1029/2003jd003428
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2003JD003428
id ftunibolognairis:oai:cris.unibo.it:11585/956459
record_format openpolar
spelling ftunibolognairis:oai:cris.unibo.it:11585/956459 2024-04-14T08:20:12+00:00 Some considerations on the infrared cloud forcing Rizzi R. Maestri T. Rizzi R. Maestri T. 2003 STAMPA https://hdl.handle.net/11585/956459 https://doi.org/10.1029/2003jd003428 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2003JD003428 eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000184603300005 volume:108 issue:14 firstpage:4403 lastpage:4408 numberofpages:6 journal:JOURNAL OF GEOPHYSICAL RESEARCH https://hdl.handle.net/11585/956459 doi:10.1029/2003jd003428 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0742270495 https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2003JD003428 Cloud forcing Infrared Radiation Radiometry info:eu-repo/semantics/article 2003 ftunibolognairis https://doi.org/10.1029/2003jd003428 2024-03-21T16:58:09Z Long-wave spectral cloud forcing is computed for realistic clouds of various optical thickness embedded in the tropical and subarctic winter standard atmospheres. The strict connections between the integrated long-wave cloud forcing (LCF) and cloud's altitude and transmissivity are shown. LCF, especially in presence of ice clouds, grows almost linearly with cloud transmissivity, and largest values are found in presence of high and opaque cirri. We have also considered the effect of incomplete spectral coverage in broadband long-wave radiometry when estimating LCF. The error has been computed as a function of edge cutoff (two different filters are used) and cloud's transmissivity and top altitude. Uncorrected measurements from sensors with incomplete spectral coverage generally underestimate the real LCF, especially for the highest cirrus clouds in the tropics. A correction is possible since the percentage error is practically constant with cloud's transmissivity. Article in Journal/Newspaper Subarctic IRIS Università degli Studi di Bologna (CRIS - Current Research Information System) Journal of Geophysical Research: Atmospheres 108 D14
institution Open Polar
collection IRIS Università degli Studi di Bologna (CRIS - Current Research Information System)
op_collection_id ftunibolognairis
language English
topic Cloud forcing
Infrared
Radiation
Radiometry
spellingShingle Cloud forcing
Infrared
Radiation
Radiometry
Rizzi R.
Maestri T.
Some considerations on the infrared cloud forcing
topic_facet Cloud forcing
Infrared
Radiation
Radiometry
description Long-wave spectral cloud forcing is computed for realistic clouds of various optical thickness embedded in the tropical and subarctic winter standard atmospheres. The strict connections between the integrated long-wave cloud forcing (LCF) and cloud's altitude and transmissivity are shown. LCF, especially in presence of ice clouds, grows almost linearly with cloud transmissivity, and largest values are found in presence of high and opaque cirri. We have also considered the effect of incomplete spectral coverage in broadband long-wave radiometry when estimating LCF. The error has been computed as a function of edge cutoff (two different filters are used) and cloud's transmissivity and top altitude. Uncorrected measurements from sensors with incomplete spectral coverage generally underestimate the real LCF, especially for the highest cirrus clouds in the tropics. A correction is possible since the percentage error is practically constant with cloud's transmissivity.
author2 Rizzi R.
Maestri T.
format Article in Journal/Newspaper
author Rizzi R.
Maestri T.
author_facet Rizzi R.
Maestri T.
author_sort Rizzi R.
title Some considerations on the infrared cloud forcing
title_short Some considerations on the infrared cloud forcing
title_full Some considerations on the infrared cloud forcing
title_fullStr Some considerations on the infrared cloud forcing
title_full_unstemmed Some considerations on the infrared cloud forcing
title_sort some considerations on the infrared cloud forcing
publishDate 2003
url https://hdl.handle.net/11585/956459
https://doi.org/10.1029/2003jd003428
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2003JD003428
genre Subarctic
genre_facet Subarctic
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000184603300005
volume:108
issue:14
firstpage:4403
lastpage:4408
numberofpages:6
journal:JOURNAL OF GEOPHYSICAL RESEARCH
https://hdl.handle.net/11585/956459
doi:10.1029/2003jd003428
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-0742270495
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2003JD003428
op_doi https://doi.org/10.1029/2003jd003428
container_title Journal of Geophysical Research: Atmospheres
container_volume 108
container_issue D14
_version_ 1796298427155349504