Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980
<p>Nadir-viewed intensities (radiances) from nine UV sensing satellite instruments are calibrated over the East Antarctic Plateau and Greenland during summer. The calibrated radiances from these UV instruments ultimately will provide a global long-term record of cloud trends and cloud response...
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doaj-6afeff8459aa4e8fa394e38518db87b32020-11-25T03:59:58ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482020-10-01135715572310.5194/amt-13-5715-2020Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980C. J. Weaver0C. J. Weaver1P. K. Bhartia2D. L. Wu3G. J. Labow4G. J. Labow5D. E. Haffner6D. E. Haffner7Atmospheric Chemistry and Dynamics Branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAEarth System Science Interdisciplinary Center (ESSIC), University of Maryland, College Park, MD 20742, USAAtmospheric Chemistry and Dynamics Branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAClimate and Radiation Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAAtmospheric Chemistry and Dynamics Branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAScience Systems and Applications (SSAI), Inc., Lanham, MD 20706, USAAtmospheric Chemistry and Dynamics Branch, NASA Goddard Space Flight Center, Greenbelt, MD 20771, USAScience Systems and Applications (SSAI), Inc., Lanham, MD 20706, USA<p>Nadir-viewed intensities (radiances) from nine UV sensing satellite instruments are calibrated over the East Antarctic Plateau and Greenland during summer. The calibrated radiances from these UV instruments ultimately will provide a global long-term record of cloud trends and cloud response from ENSO events since 1980. We first remove the strong solar zenith angle dependence from the intensities using an empirical approach rather than a radiative transfer model. Then small multiplicative adjustments are made to these solar zenith angle normalized intensities in order to minimize differences when two or more instruments temporally overlap. While the calibrated intensities show a negligible long-term trend over Antarctica and a statistically insignificant UV albedo trend of <span class="inline-formula">−0.05</span> % per decade over the interior of Greenland, there are small episodic reductions in intensities which are often seen by multiple instruments. Three of these darkening events are explained by boreal forest. Other events are caused by surface melting or volcanoes. We estimate a 2-sigma uncertainty of 0.35 % for the calibrated radiances.</p>https://amt.copernicus.org/articles/13/5715/2020/amt-13-5715-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
C. J. Weaver C. J. Weaver P. K. Bhartia D. L. Wu G. J. Labow G. J. Labow D. E. Haffner D. E. Haffner |
spellingShingle |
C. J. Weaver C. J. Weaver P. K. Bhartia D. L. Wu G. J. Labow G. J. Labow D. E. Haffner D. E. Haffner Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 Atmospheric Measurement Techniques |
author_facet |
C. J. Weaver C. J. Weaver P. K. Bhartia D. L. Wu G. J. Labow G. J. Labow D. E. Haffner D. E. Haffner |
author_sort |
C. J. Weaver |
title |
Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 |
title_short |
Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 |
title_full |
Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 |
title_fullStr |
Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 |
title_full_unstemmed |
Inter-calibration of nine UV sensing instruments over Antarctica and Greenland since 1980 |
title_sort |
inter-calibration of nine uv sensing instruments over antarctica and greenland since 1980 |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2020-10-01 |
description |
<p>Nadir-viewed intensities (radiances) from nine UV sensing satellite
instruments are calibrated over the East Antarctic Plateau and Greenland
during summer. The calibrated radiances from these UV instruments ultimately
will provide a global long-term record of cloud trends and cloud response
from ENSO events since 1980. We first remove the strong solar zenith angle
dependence from the intensities using an empirical approach rather than a
radiative transfer model. Then small multiplicative adjustments are made to
these solar zenith angle normalized intensities in order to minimize
differences when two or more instruments temporally overlap. While the
calibrated intensities show a negligible long-term trend over Antarctica and a statistically insignificant UV albedo trend of <span class="inline-formula">−0.05</span> % per decade
over the interior of Greenland, there are small episodic reductions
in intensities which are often seen by multiple instruments. Three of these
darkening events are explained by boreal forest. Other events are caused by
surface melting or volcanoes. We estimate a 2-sigma uncertainty of 0.35 %
for the calibrated radiances.</p> |
url |
https://amt.copernicus.org/articles/13/5715/2020/amt-13-5715-2020.pdf |
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