ENSO surface shortwave radiation forcing over the tropical Pacific

We have studied the spatial and temporal variation of the downward shortwave radiation (DSR) at the surface of the Earth during ENSO events for a 21-year period over the tropical and subtropical Pacific Ocean (40° S–40° N, 90° E–75° W). The fluxes were...

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Main Authors: K. G. Pavlakis, N. Hatzianastassiou, C. Matsoukas, A. Fotiadi, I. Vardavas
Format: Article
Language:English
Published: Copernicus Publications 2008-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/5565/2008/acp-8-5565-2008.pdf
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author K. G. Pavlakis
N. Hatzianastassiou
C. Matsoukas
A. Fotiadi
I. Vardavas
author_facet K. G. Pavlakis
N. Hatzianastassiou
C. Matsoukas
A. Fotiadi
I. Vardavas
author_sort K. G. Pavlakis
collection DOAJ
description We have studied the spatial and temporal variation of the downward shortwave radiation (DSR) at the surface of the Earth during ENSO events for a 21-year period over the tropical and subtropical Pacific Ocean (40° S–40° N, 90° E–75° W). The fluxes were computed using a deterministic model for atmospheric radiation transfer, along with satellite data from the ISCCP-D2 database, reanalysis data from NCEP/NCAR for the key atmospheric and surface input parameters, and aerosol parameters from GADS (acronyms explained in main text). A clear anti-correlation was found between the downward shortwave radiation anomaly (DSR-A) time-series, in the region 7° S–5° N 160° E–160° W located west of the Niño-3.4 region, and the Niño-3.4 index time-series. In this region where the highest in absolute value DSR anomalies are observed, the mean DSR anomaly values range from −45 Wm<sup>−2</sup> during El Niño episodes to +40 Wm<sup>−2</sup> during La Niña events. Within the Niño-3.4 region no significant DSR anomalies are observed during the cold ENSO phase in contrast to the warm ENSO phase. A high correlation was also found over the western Pacific (10° S–5° N, 120–140° E), where the mean DSR anomaly values range from +20 Wm<sup>−2</sup> to −20 Wm<sup>−2</sup> during El Niño and La Niña episodes, respectively. There is also convincing evidence that the time series of the mean downward shortwave radiation anomaly in the off-equatorial western Pacific region 7–15° N 150–170° E, precedes the Niño-3.4 index time-series by about 7 months and the pattern of this anomaly is indicative of ENSO operating through the mechanism of the western Pacific oscillator. Thus, the downward shortwave radiation anomaly is a complementary index to the SST anomaly for the study of ENSO events and can be used to assess whether or not El Niño or La Niña conditions prevail.
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spelling doaj.art-d9574c490c4640c59dfb16f6a993eb712022-12-22T00:48:31ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-09-0181855655577ENSO surface shortwave radiation forcing over the tropical PacificK. G. PavlakisN. HatzianastassiouC. MatsoukasA. FotiadiI. VardavasWe have studied the spatial and temporal variation of the downward shortwave radiation (DSR) at the surface of the Earth during ENSO events for a 21-year period over the tropical and subtropical Pacific Ocean (40° S–40° N, 90° E–75° W). The fluxes were computed using a deterministic model for atmospheric radiation transfer, along with satellite data from the ISCCP-D2 database, reanalysis data from NCEP/NCAR for the key atmospheric and surface input parameters, and aerosol parameters from GADS (acronyms explained in main text). A clear anti-correlation was found between the downward shortwave radiation anomaly (DSR-A) time-series, in the region 7° S–5° N 160° E–160° W located west of the Niño-3.4 region, and the Niño-3.4 index time-series. In this region where the highest in absolute value DSR anomalies are observed, the mean DSR anomaly values range from −45 Wm<sup>−2</sup> during El Niño episodes to +40 Wm<sup>−2</sup> during La Niña events. Within the Niño-3.4 region no significant DSR anomalies are observed during the cold ENSO phase in contrast to the warm ENSO phase. A high correlation was also found over the western Pacific (10° S–5° N, 120–140° E), where the mean DSR anomaly values range from +20 Wm<sup>−2</sup> to −20 Wm<sup>−2</sup> during El Niño and La Niña episodes, respectively. There is also convincing evidence that the time series of the mean downward shortwave radiation anomaly in the off-equatorial western Pacific region 7–15° N 150–170° E, precedes the Niño-3.4 index time-series by about 7 months and the pattern of this anomaly is indicative of ENSO operating through the mechanism of the western Pacific oscillator. Thus, the downward shortwave radiation anomaly is a complementary index to the SST anomaly for the study of ENSO events and can be used to assess whether or not El Niño or La Niña conditions prevail.http://www.atmos-chem-phys.net/8/5565/2008/acp-8-5565-2008.pdf
spellingShingle K. G. Pavlakis
N. Hatzianastassiou
C. Matsoukas
A. Fotiadi
I. Vardavas
ENSO surface shortwave radiation forcing over the tropical Pacific
Atmospheric Chemistry and Physics
title ENSO surface shortwave radiation forcing over the tropical Pacific
title_full ENSO surface shortwave radiation forcing over the tropical Pacific
title_fullStr ENSO surface shortwave radiation forcing over the tropical Pacific
title_full_unstemmed ENSO surface shortwave radiation forcing over the tropical Pacific
title_short ENSO surface shortwave radiation forcing over the tropical Pacific
title_sort enso surface shortwave radiation forcing over the tropical pacific
url http://www.atmos-chem-phys.net/8/5565/2008/acp-8-5565-2008.pdf
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