Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies
The High-Resolution Infrared Radiation Sounder (HIRS) on NOAA and MetOp A/B satellites has been observing the Earth continuously for over four decades, providing essential data for operational numerical weather prediction, retrieval of atmospheric vertical profile, and total column information on at...
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MDPI AG
2021-10-01
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author | Bin Zhang Changyong Cao Tung-Chang Liu Xi Shao |
author_facet | Bin Zhang Changyong Cao Tung-Chang Liu Xi Shao |
author_sort | Bin Zhang |
collection | DOAJ |
description | The High-Resolution Infrared Radiation Sounder (HIRS) on NOAA and MetOp A/B satellites has been observing the Earth continuously for over four decades, providing essential data for operational numerical weather prediction, retrieval of atmospheric vertical profile, and total column information on atmospheric temperature, moisture, water vapor, ozone, cloud climatology, and other geophysical parameters globally. Although the HIRS data meets the needs of the short-term weather forecast, there are inconsistencies when the long-term decadal time series is used for time series analysis. The discrepancies are caused by several factors, including spectral response differences between the HIRS models on the satellites and spectral response uncertainties and other calibration issues. Previous studies have demonstrated that significant improvements can be achieved by recalibrating some of the HIRS longwave CO<sub>2</sub> channels (Channels 4, 5, 6, and 7), which has helped make the time series more consistent. The current study aims to extend the previous study to the remaining longwave infrared sounding channels, including Channels 1, 2, 3, and 8, using a similar approach. Similar to previous findings, the spectral shift of the HIRS bands has helped improve the consistency in the time series from NOAA-06 to MetOp-A and B for these channels. We also found that HIRS channels on MetOp-B also have bias relative to Infrared Atmospheric Sounding Interferometer (IASI) on the same satellite, especially Channel 4, and a spectral shift significantly reduced the bias. To bridge the observation gap in time series in the mid-1980s between NOAA-07 and NOAA-09, the global mean method has been used since no transfer radiometers between them was available for this period, and the spectral response function corrections, therefore, can be applied to the earliest satellites (NOAA-06) for these channels. The recalibration parameters have been provided to other scientists at the University of Wisconsin for improving the time series in their long-term studies using historical HIRS data and are now made available to the science community. |
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spelling | doaj.art-583262bf7ad64711926f733f46f9f1e42023-11-22T17:25:42ZengMDPI AGAtmosphere2073-44332021-10-011210131710.3390/atmos12101317Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate StudiesBin Zhang0Changyong Cao1Tung-Chang Liu2Xi Shao3Earth System Science Interdisciplinary Center, Cooperative Institute for Satellite Earth System Studies (CISESS), University of Maryland, College Park, MD 20740, USACenter for Satellite Applications and Research, NOAA National Environmental Satellite, Data, and Information Service, College Park, MD 20740, USAEarth System Science Interdisciplinary Center, Cooperative Institute for Satellite Earth System Studies (CISESS), University of Maryland, College Park, MD 20740, USAEarth System Science Interdisciplinary Center, Cooperative Institute for Satellite Earth System Studies (CISESS), University of Maryland, College Park, MD 20740, USAThe High-Resolution Infrared Radiation Sounder (HIRS) on NOAA and MetOp A/B satellites has been observing the Earth continuously for over four decades, providing essential data for operational numerical weather prediction, retrieval of atmospheric vertical profile, and total column information on atmospheric temperature, moisture, water vapor, ozone, cloud climatology, and other geophysical parameters globally. Although the HIRS data meets the needs of the short-term weather forecast, there are inconsistencies when the long-term decadal time series is used for time series analysis. The discrepancies are caused by several factors, including spectral response differences between the HIRS models on the satellites and spectral response uncertainties and other calibration issues. Previous studies have demonstrated that significant improvements can be achieved by recalibrating some of the HIRS longwave CO<sub>2</sub> channels (Channels 4, 5, 6, and 7), which has helped make the time series more consistent. The current study aims to extend the previous study to the remaining longwave infrared sounding channels, including Channels 1, 2, 3, and 8, using a similar approach. Similar to previous findings, the spectral shift of the HIRS bands has helped improve the consistency in the time series from NOAA-06 to MetOp-A and B for these channels. We also found that HIRS channels on MetOp-B also have bias relative to Infrared Atmospheric Sounding Interferometer (IASI) on the same satellite, especially Channel 4, and a spectral shift significantly reduced the bias. To bridge the observation gap in time series in the mid-1980s between NOAA-07 and NOAA-09, the global mean method has been used since no transfer radiometers between them was available for this period, and the spectral response function corrections, therefore, can be applied to the earliest satellites (NOAA-06) for these channels. The recalibration parameters have been provided to other scientists at the University of Wisconsin for improving the time series in their long-term studies using historical HIRS data and are now made available to the science community.https://www.mdpi.com/2073-4433/12/10/1317HIRS longwave CO<sub>2</sub> channelHIRS SRF calibrationHIRS SNOglobal meanSRF shift |
spellingShingle | Bin Zhang Changyong Cao Tung-Chang Liu Xi Shao Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies Atmosphere HIRS longwave CO<sub>2</sub> channel HIRS SRF calibration HIRS SNO global mean SRF shift |
title | Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies |
title_full | Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies |
title_fullStr | Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies |
title_full_unstemmed | Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies |
title_short | Spectral Recalibration of NOAA HIRS Longwave CO<sub>2</sub> Channels toward a 40+ Year Time Series for Climate Studies |
title_sort | spectral recalibration of noaa hirs longwave co sub 2 sub channels toward a 40 year time series for climate studies |
topic | HIRS longwave CO<sub>2</sub> channel HIRS SRF calibration HIRS SNO global mean SRF shift |
url | https://www.mdpi.com/2073-4433/12/10/1317 |
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