Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties

Information content analysis is used to select channels for a marine liquid cloud retrieval using the high-spectral-resolution oxygen A-band instrument on NASA's Orbiting Carbon Observatory-2 (OCO-2). Desired retrieval properties are cloud optical depth, cloud-top pressure and cloud pressur...

Full description

Bibliographic Details
Main Authors: M. Richardson, G. L. Stephens
Format: Article
Language:English
Published: Copernicus Publications 2018-03-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/11/1515/2018/amt-11-1515-2018.pdf
id doaj-fba4c0fdd259473fa1b59da147169ebf
record_format Article
spelling doaj-fba4c0fdd259473fa1b59da147169ebf2020-11-24T22:53:47ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482018-03-01111515152810.5194/amt-11-1515-2018Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud propertiesM. Richardson0G. L. Stephens1G. L. Stephens2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91125, USAJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91125, USADepartment of Meteorology, University of Reading, Reading, RG6 6BB, UKInformation content analysis is used to select channels for a marine liquid cloud retrieval using the high-spectral-resolution oxygen A-band instrument on NASA's Orbiting Carbon Observatory-2 (OCO-2). Desired retrieval properties are cloud optical depth, cloud-top pressure and cloud pressure thickness, which is the geometric thickness expressed in hectopascals. Based on information content criteria we select a micro-window of 75 of the 853 functioning OCO-2 channels spanning 763.5–764.6 nm and perform a series of synthetic retrievals with perturbed initial conditions. We estimate posterior errors from the sample standard deviations and obtain ±0.75 in optical depth and ±12.9 hPa in both cloud-top pressure and cloud pressure thickness, although removing the 10 % of samples with the highest <i>χ</i><sup>2</sup> reduces posterior error in cloud-top pressure to ±2.9 hPa and cloud pressure thickness to ±2.5 hPa. The application of this retrieval to real OCO-2 measurements is briefly discussed, along with limitations and the greatest caution is urged regarding the assumption of a single homogeneous cloud layer, which is often, but not always, a reasonable approximation for marine boundary layer clouds.https://www.atmos-meas-tech.net/11/1515/2018/amt-11-1515-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Richardson
G. L. Stephens
G. L. Stephens
spellingShingle M. Richardson
G. L. Stephens
G. L. Stephens
Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
Atmospheric Measurement Techniques
author_facet M. Richardson
G. L. Stephens
G. L. Stephens
author_sort M. Richardson
title Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
title_short Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
title_full Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
title_fullStr Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
title_full_unstemmed Information content of OCO-2 oxygen A-band channels for retrieving marine liquid cloud properties
title_sort information content of oco-2 oxygen a-band channels for retrieving marine liquid cloud properties
publisher Copernicus Publications
series Atmospheric Measurement Techniques
issn 1867-1381
1867-8548
publishDate 2018-03-01
description Information content analysis is used to select channels for a marine liquid cloud retrieval using the high-spectral-resolution oxygen A-band instrument on NASA's Orbiting Carbon Observatory-2 (OCO-2). Desired retrieval properties are cloud optical depth, cloud-top pressure and cloud pressure thickness, which is the geometric thickness expressed in hectopascals. Based on information content criteria we select a micro-window of 75 of the 853 functioning OCO-2 channels spanning 763.5–764.6 nm and perform a series of synthetic retrievals with perturbed initial conditions. We estimate posterior errors from the sample standard deviations and obtain ±0.75 in optical depth and ±12.9 hPa in both cloud-top pressure and cloud pressure thickness, although removing the 10 % of samples with the highest <i>χ</i><sup>2</sup> reduces posterior error in cloud-top pressure to ±2.9 hPa and cloud pressure thickness to ±2.5 hPa. The application of this retrieval to real OCO-2 measurements is briefly discussed, along with limitations and the greatest caution is urged regarding the assumption of a single homogeneous cloud layer, which is often, but not always, a reasonable approximation for marine boundary layer clouds.
url https://www.atmos-meas-tech.net/11/1515/2018/amt-11-1515-2018.pdf
work_keys_str_mv AT mrichardson informationcontentofoco2oxygenabandchannelsforretrievingmarineliquidcloudproperties
AT glstephens informationcontentofoco2oxygenabandchannelsforretrievingmarineliquidcloudproperties
AT glstephens informationcontentofoco2oxygenabandchannelsforretrievingmarineliquidcloudproperties
_version_ 1725661833017163776