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...
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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 |
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