The Extraordinary Equatorial Atlantic Warming in Late 2019
Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this variability has shown comparatively little activity. In late 2019, however, the warmest event in the satellite observation period developed. Anal...
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| Published in: | Geophysical research letters Vol. 49; no. 4 |
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| Main Authors: | , , |
| Format: | Journal Article |
| Language: | English |
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John Wiley & Sons, Inc
28.02.2022
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| ISSN: | 0094-8276, 1944-8007 |
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| Abstract | Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this variability has shown comparatively little activity. In late 2019, however, the warmest event in the satellite observation period developed. Analysis suggests that zonal wind stress anomalies in the western equatorial Atlantic contributed to the development of the warm SST anomalies. Furthermore, wind stress curl anomalies north of the equator generated downwelling Rossby waves that propagated to the western boundary and were reflected into downwelling Kelvin waves that helped to precondition the event. Neither the contemporaneous positive Indian Ocean Dipole nor the El Niño Modoki appears to have contributed substantially to the Atlantic warming, though some uncertainty remains. Based on large‐scale multidecadal variability patterns, a return to enhanced variability is not imminent but careful monitoring will be important.
Plain Language Summary
Year‐to‐year variability of ocean surface temperatures in the eastern equatorial Atlantic has been relatively weak over the last 20 years. In late 2019, however, an exceptionally strong event developed. This event appears to have been generated by surface wind stress forcing both on and north of the equator. Remote influences from other tropical basins do not seem to have played a large role. Based on large‐scale multidecadal variability patterns in the region, the equatorial Atlantic may return to relatively low variability but continued monitoring will be important.
Key Points
One of the strongest equatorial Atlantic warm events of the last 40 years developed in late 2019
Wind stress forcing both on and off the equator contributed to the exceptionally strong warming
Analysis suggests that remote forcing from other basins was not a major factor in the genesis of the event |
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| AbstractList | Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this variability has shown comparatively little activity. In late 2019, however, the warmest event in the satellite observation period developed. Analysis suggests that zonal wind stress anomalies in the western equatorial Atlantic contributed to the development of the warm SST anomalies. Furthermore, wind stress curl anomalies north of the equator generated downwelling Rossby waves that propagated to the western boundary and were reflected into downwelling Kelvin waves that helped to precondition the event. Neither the contemporaneous positive Indian Ocean Dipole nor the El Niño Modoki appears to have contributed substantially to the Atlantic warming, though some uncertainty remains. Based on large‐scale multidecadal variability patterns, a return to enhanced variability is not imminent but careful monitoring will be important.
Plain Language Summary
Year‐to‐year variability of ocean surface temperatures in the eastern equatorial Atlantic has been relatively weak over the last 20 years. In late 2019, however, an exceptionally strong event developed. This event appears to have been generated by surface wind stress forcing both on and north of the equator. Remote influences from other tropical basins do not seem to have played a large role. Based on large‐scale multidecadal variability patterns in the region, the equatorial Atlantic may return to relatively low variability but continued monitoring will be important.
Key Points
One of the strongest equatorial Atlantic warm events of the last 40 years developed in late 2019
Wind stress forcing both on and off the equator contributed to the exceptionally strong warming
Analysis suggests that remote forcing from other basins was not a major factor in the genesis of the event Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this variability has shown comparatively little activity. In late 2019, however, the warmest event in the satellite observation period developed. Analysis suggests that zonal wind stress anomalies in the western equatorial Atlantic contributed to the development of the warm SST anomalies. Furthermore, wind stress curl anomalies north of the equator generated downwelling Rossby waves that propagated to the western boundary and were reflected into downwelling Kelvin waves that helped to precondition the event. Neither the contemporaneous positive Indian Ocean Dipole nor the El Niño Modoki appears to have contributed substantially to the Atlantic warming, though some uncertainty remains. Based on large‐scale multidecadal variability patterns, a return to enhanced variability is not imminent but careful monitoring will be important. Year‐to‐year variability of ocean surface temperatures in the eastern equatorial Atlantic has been relatively weak over the last 20 years. In late 2019, however, an exceptionally strong event developed. This event appears to have been generated by surface wind stress forcing both on and north of the equator. Remote influences from other tropical basins do not seem to have played a large role. Based on large‐scale multidecadal variability patterns in the region, the equatorial Atlantic may return to relatively low variability but continued monitoring will be important. One of the strongest equatorial Atlantic warm events of the last 40 years developed in late 2019 Wind stress forcing both on and off the equator contributed to the exceptionally strong warming Analysis suggests that remote forcing from other basins was not a major factor in the genesis of the event Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this variability has shown comparatively little activity. In late 2019, however, the warmest event in the satellite observation period developed. Analysis suggests that zonal wind stress anomalies in the western equatorial Atlantic contributed to the development of the warm SST anomalies. Furthermore, wind stress curl anomalies north of the equator generated downwelling Rossby waves that propagated to the western boundary and were reflected into downwelling Kelvin waves that helped to precondition the event. Neither the contemporaneous positive Indian Ocean Dipole nor the El Niño Modoki appears to have contributed substantially to the Atlantic warming, though some uncertainty remains. Based on large‐scale multidecadal variability patterns, a return to enhanced variability is not imminent but careful monitoring will be important. |
| Author | Richter, Ingo Okumura, Yuko M. Tokinaga, Hiroki |
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| Cites_doi | 10.1029/2010GL044461 10.1002/joc.4775 10.1175/JCLI-D-11-00553.1 10.1038/s41467-020-20452-1 10.1029/2020GL087108 10.1175/JCLI3812.1 10.1029/2002JD002670 10.1175/JCLI-D-16-0836.1 10.1175/jcli3992.1 10.1029/2006JC003798 10.1029/2006GL026894 10.1038/43854 10.1002/2016JC011719 10.1002/qj.3803 10.1175/JCLI-D-20-0166.1 10.1007/s00382-020-05605-8 10.1175/1520-0442(2004)017<3589:IOTAEC>2.0.CO;2 10.1007/s00382-016-3289-y 10.1175/jcli4189.1 10.1175/1520-0493(1969)097<0163:atftep>2.3.co;2 10.1175/JCLI-D-15-0894.1 10.1029/2019GL086713 10.1002/joc.1169 10.1175/JCLI-D-16-0816.1 10.1038/ngeo1078 10.1007/s00382-020-05138-0 10.1016/B978-0-12-818156-0.00008-3 10.1175/jcli3928.1 10.1029/1999GL900014 10.1175/1525-7541(2003)004<1147:tvgpcp>2.0.co;2 10.1029/2021GL092489 10.2151/jmsj.2015-001 10.1029/2000GL012745 10.1175/JCLI-D-16-0459.1 10.1038/ngeo1660 10.1007/s00382-020-05409-w 10.1007/s00382-014-2168-7 10.1038/s41467-021-26223-w 10.1175/1520-0477(2001)082<0247:tnnyrm>2.3.co;2 10.1029/2010gl045522 10.1038/s41598-017-11046-x 10.1029/2009JC005964 10.1175/1520-0469(1999)056<0374:CCEWAO>2.0.CO;2 10.1175/1520-0493(1987)115<2262:ameno>2.0.co;2 10.1029/2018EA000428 10.3389/fmars.2021.800103 |
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| References | e_1_2_8_1_12_1 e_1_2_8_1_35_1 e_1_2_8_1_11_1 e_1_2_8_1_36_1 e_1_2_8_1_14_1 e_1_2_8_1_33_1 e_1_2_8_1_13_1 e_1_2_8_1_34_1 e_1_2_8_1_31_1 e_1_2_8_1_32_1 e_1_2_8_1_10_1 e_1_2_8_1_30_1 e_1_2_8_1_8_1 e_1_2_8_1_9_1 Merle J. (e_1_2_8_1_22_1) 1980; 3 e_1_2_8_2_7_1 e_1_2_8_2_8_1 e_1_2_8_2_9_1 e_1_2_8_1_27_1 e_1_2_8_1_26_1 e_1_2_8_1_29_1 e_1_2_8_1_28_1 e_1_2_8_1_23_1 Liebmann B. (e_1_2_8_1_18_1) 1996; 77 e_1_2_8_1_25_1 e_1_2_8_1_24_1 e_1_2_8_2_2_1 e_1_2_8_2_3_1 e_1_2_8_2_4_1 e_1_2_8_1_21_1 e_1_2_8_2_5_1 e_1_2_8_1_20_1 e_1_2_8_2_6_1 e_1_2_8_2_10_1 e_1_2_8_2_11_1 e_1_2_8_1_2_1 e_1_2_8_1_3_1 e_1_2_8_1_6_1 e_1_2_8_1_7_1 e_1_2_8_1_4_1 e_1_2_8_1_5_1 e_1_2_8_1_19_1 e_1_2_8_1_16_1 e_1_2_8_1_39_1 e_1_2_8_1_15_1 e_1_2_8_1_37_1 e_1_2_8_1_17_1 e_1_2_8_1_38_1 |
| References_xml | – ident: e_1_2_8_1_28_1 doi: 10.1029/2010GL044461 – ident: e_1_2_8_2_4_1 doi: 10.1002/joc.4775 – ident: e_1_2_8_1_20_1 doi: 10.1175/JCLI-D-11-00553.1 – ident: e_1_2_8_1_23_1 doi: 10.1038/s41467-020-20452-1 – ident: e_1_2_8_1_37_1 doi: 10.1029/2020GL087108 – ident: e_1_2_8_2_9_1 doi: 10.1175/JCLI3812.1 – ident: e_1_2_8_2_8_1 doi: 10.1029/2002JD002670 – ident: e_1_2_8_2_6_1 doi: 10.1175/JCLI-D-16-0836.1 – volume: 77 start-page: 1275 year: 1996 ident: e_1_2_8_1_18_1 article-title: Description of a complete (interpolated) outgoing longwave radiation dataset publication-title: Bulletin of the American Meteorological Society – ident: e_1_2_8_1_14_1 doi: 10.1175/jcli3992.1 – ident: e_1_2_8_1_3_1 doi: 10.1029/2006JC003798 – ident: e_1_2_8_2_10_1 doi: 10.1029/2006GL026894 – ident: e_1_2_8_1_33_1 doi: 10.1038/43854 – ident: e_1_2_8_1_6_1 doi: 10.1002/2016JC011719 – ident: e_1_2_8_2_5_1 doi: 10.1002/qj.3803 – ident: e_1_2_8_1_12_1 doi: 10.1175/JCLI-D-20-0166.1 – ident: e_1_2_8_1_7_1 doi: 10.1007/s00382-020-05605-8 – ident: e_1_2_8_1_25_1 doi: 10.1175/1520-0442(2004)017<3589:IOTAEC>2.0.CO;2 – ident: e_1_2_8_1_32_1 doi: 10.1007/s00382-016-3289-y – ident: e_1_2_8_1_11_1 doi: 10.1175/jcli4189.1 – ident: e_1_2_8_1_4_1 doi: 10.1175/1520-0493(1969)097<0163:atftep>2.3.co;2 – ident: e_1_2_8_1_24_1 doi: 10.1175/JCLI-D-15-0894.1 – volume: 3 start-page: 209 year: 1980 ident: e_1_2_8_1_22_1 article-title: Annual and interannual variability of temperature in the eastern equatorial Atlantic Ocean – Hypothesis of an Atlantic El Nino publication-title: Oceanologica Acta – ident: e_1_2_8_1_8_1 doi: 10.1029/2019GL086713 – ident: e_1_2_8_2_7_1 doi: 10.1002/joc.1169 – ident: e_1_2_8_1_10_1 doi: 10.1175/JCLI-D-16-0816.1 – ident: e_1_2_8_1_36_1 doi: 10.1038/ngeo1078 – ident: e_1_2_8_1_27_1 doi: 10.1007/s00382-020-05138-0 – ident: e_1_2_8_1_31_1 doi: 10.1016/B978-0-12-818156-0.00008-3 – ident: e_1_2_8_1_26_1 doi: 10.1175/jcli3928.1 – ident: e_1_2_8_1_35_1 doi: 10.1029/1999GL900014 – ident: e_1_2_8_1_2_1 doi: 10.1175/1525-7541(2003)004<1147:tvgpcp>2.0.co;2 – ident: e_1_2_8_1_17_1 doi: 10.1029/2021GL092489 – ident: e_1_2_8_1_16_1 doi: 10.2151/jmsj.2015-001 – ident: e_1_2_8_2_2_1 doi: 10.1029/2000GL012745 – ident: e_1_2_8_1_21_1 doi: 10.1175/JCLI-D-16-0459.1 – ident: e_1_2_8_1_29_1 doi: 10.1038/ngeo1660 – ident: e_1_2_8_1_30_1 doi: 10.1007/s00382-020-05409-w – ident: e_1_2_8_1_34_1 doi: 10.1007/s00382-014-2168-7 – ident: e_1_2_8_1_39_1 doi: 10.1038/s41467-021-26223-w – ident: e_1_2_8_1_15_1 doi: 10.1175/1520-0477(2001)082<0247:tnnyrm>2.3.co;2 – ident: e_1_2_8_1_9_1 doi: 10.1029/2010gl045522 – ident: e_1_2_8_2_3_1 doi: 10.1038/s41598-017-11046-x – ident: e_1_2_8_1_19_1 doi: 10.1029/2009JC005964 – ident: e_1_2_8_2_11_1 doi: 10.1175/1520-0469(1999)056<0374:CCEWAO>2.0.CO;2 – ident: e_1_2_8_1_38_1 doi: 10.1175/1520-0493(1987)115<2262:ameno>2.0.co;2 – ident: e_1_2_8_1_5_1 doi: 10.1029/2018EA000428 – ident: e_1_2_8_1_13_1 doi: 10.3389/fmars.2021.800103 |
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| Snippet | Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this... Sea‐surface temperatures (SSTs) in the eastern equatorial Atlantic are subject to variability on interannual timescales but during the last 20 years, this... |
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| SubjectTerms | Anomalies Atlantic Nino Atlantic zonal mode Dipoles Downwelling El Nino El Nino phenomena Equator equatorial Atlantic Equatorial regions interannual variability IOD Kelvin waves Monitoring Ocean surface Ocean temperature Oceans Planetary waves Rossby waves Satellite observation Sea surface Sea surface temperature Sea surface temperature anomalies Surface temperature Surface wind Tropical climate Variability Wave propagation Wind stress Wind stress curl Zonal winds |
| Title | The Extraordinary Equatorial Atlantic Warming in Late 2019 |
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