Caniaux g 20150707_1700_upmc_jussieu_-_room_201
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Transcript of Caniaux g 20150707_1700_upmc_jussieu_-_room_201
Origin of the Recent Tropical Atlantic SST warming:
the role of ocean dynamics?
J. Servain1,3, G. Caniaux2, G.A. Hounsou-Gbo3,
Y.K. Kouadio4, M.J. McPhaden5, and M. Araújo3
1. IRD/LOCEAN, 4 Place Jussieu, Paris, FRANCE
2. CNRM/GAME (Météo-France/CNRS), Toulouse, FRANCE
3. Universidade Federal de Pernambouco, Recife-PE, BRAZIL
4. LPA, Université de Cocody, Abidjan, IVORY COAST
5. PMEL/NOAA, Seattle-WA, U.S.A.
Introduction
•Observed oceanic trends in part reflect our changing climate •The intensity of the long-term SST warming is different depending on ocean bassin and the period of reference: -between 1850 and 2004: NH +0.59°C and SH +0.46°C [Rayner et al., 2006] -between 1956 and 2004, the Atlantic ocean gained +0.059°C/decade; +0.043°C/decade elsewhere [Palmer et al., 2007] •Here we focus mainly on the tropical Atlantic ocean and recent long-term climatic trends, by using a coherent data set (SST and winds) , mainly from VOS since 1964 [Servain et al., 1985]
SST anomalies +0.7°C over 48 years
Pseudo wind stress (PWS) anomalies
+12 m²/s² over 48 years
Temperature and wind tendencies
SERV Mean SST and PWS
1964-2012
•Data base SERV:~6000 observations since January 1964 •Monthly grided SST and pseudo-wind stress (2°x2°), objectively analyzed on 2°x2° boxes with a method based on
Cressman [1959] •Available at: http://www.funceme.br/index.php/areas/oceanografia/campos-numericos-do-atlantico
SST/PWS SERV
1964-1975
SST/PWS SERV
1976-2012
SST and PWS: regional analysis
•Decrease of the total change (linear regression trends x length of the series) down to -1.2°C in the NH, in agreement with the wind increase (~+10m²/s²) •Slow warming (+0.5°C but locally up to +0.8°C) in the SH
Significant SST change (max: +1.6°C) and PWS
strengthening (up to 20 m²/s² along the African coast) over
the whole basin
AT OAFlux
1976-2012
Comparison with other data sets: AT and SST
AT anomalies I-COADS [Woodruff et al., 2011] OAFlux [Yu and Weller, 2007] TropFlux [Kumar et al., 2012] SST anomalies SERV
Similar to the regional pattern
of SSTs
Significant warming since the 1970’s and similar interannual variability
Surface wind tendencies I-COADS [Woodruff et al., 2011]
OAFlux [Yu and Weller, 2007] WASWind [Tokinaga and Xie, 2011]
TropFlux [Kumar et al., 2012]
Normalized Serv PWS and TropFlux wind-stress
tendencies
Comparison of surface winds and PWS
Long-term increase in wind magnitude (resp. +0.17 m/s, +0.06 m/s, +0.06 m/s, +0.02 m/s per decade),
wind-stress (+6.5x10-4 N/m²) and PWS (+2.7 m²/s²)
PWS SERV
1964-1975
WASWinds 1964-1975
OAFlux 1964-1975
PWS and wind tendencies : regional analysis
•Intensification of the winds and PWS in the NH in all the three data sets •The change in the SH is less consistent, but relatively similar between SERV and OAFlux
NHF TropFlux
1976-2012
NHF I-COADS
1976-2012
Origin of SST tendencies: surface heat fluxes
Surface net heat fluxes I-COADS TropFlux OAFlux
Decomposition of the NHF
TropFlux Latent heat fluxes
PIRATA buoys network
x x x x x x x x
x x
Origin of SST tendencies: in-situ data
Section at 38°W
Section at 0°N
Section at 10°W
Tendencies 1998-2012
S N
N S
W E
Origin of SST tendencies: mean sea level
SLA AVISO
1993-2012
4-6 cm over the whole area max values (10 cm) in the NH
around the ITCZ
1993
Normalized 12-month moving averages of SERV SST and SLA anomalies
•Positive MSL long-term trend clearly related to the long- term trend of SST •Good correspondance between MSL and SST variability (Corr = 0.5 for the detrended non-smoothed series)
EN3 HC 0-700m 1964-2012
Origin of SST tendencies: heat content 0-700 m
0
700m
dzHC in °C.m
Normalized 12-month moving averages of SERV SST and EN3 heat content anomalies EN3 (Ingleby and Huddleston, 2007): ECMWF analysis since 1950
•Marked warming in the HC similar to Palmer et al. (2007) i.e. +30 °Cm/decade •Stronger trend in the N and E of the area where SST changes are the strongest
Conclusions
•SST increase of 0.7°C between 1976-2012 and simultaneous PWS increase of +12 m²/s² over the last five decades •The tendencies are confirmed over other independent parameters (AT, SLA) and other data sets •(1) The negative tendency of surface net heat flux, (2) the positive tendencies of the upper thermocline temperatures (PIRATA buoys), (3) of SLA, (4) of the 0-700 m heat content, tend to prove that the oceanic dynamics is the main actor of the equatorial SST warming •Role of the AMOC (suggested by Rahmstorf et al. [2013], Grist et al. [2010], Wen et al. [2010, 2011], Desbruyères et al. [2013]), role of STCs [Kröger et al., 2005], role of the Agulhas leakage and the Indian Ocean [Lee et al., 2011; Rühs et al., 2013; Shen and Tung, 2014]?