shenfu dong cimas/um and noaa/aoml
DESCRIPTION
The Role of Inter-ocean Exchanges on Long-term Variability of the Northward Heat Transport in the South Atlantic. Shenfu Dong CIMAS/UM and NOAA/AOML. S. L. Garzoli, M.Baringer NOAA/AOML, Miami, Florida USA. June 9, 2010. R. Lumpkin, NOAA/AOML. Objective: - PowerPoint PPT PresentationTRANSCRIPT
The Role of Inter-ocean Exchanges on Long-term Variability of the Northward Heat
Transport in the South Atlantic
Shenfu DongShenfu DongCIMAS/UM and NOAA/AOML
S. L. Garzoli, M.BaringerNOAA/AOML, Miami, Florida USA
June 9, 2010
R. Lumpkin, NOAA/AOML
Objective:
To investigate the role of the inter-ocean exchanges in the variability of the northward heat transport in the South Atlantic.
Specific Question: Where does the variability in the northward heat transport come from?
• Inter-ocean exchanges with the Pacific Ocean.• Inter-ocean exchanges with the Indian Ocean.• Air-sea heat exchanges.• heat storage in the basin.
SAfricaDrake HTHTHTQthc
35
AfricaDrakeS HTHTQthc
HT 35
OGCM for the Earth Simulator (OFES)
The model code is based on MOM3. OFES covers 75S to 75N. 0.1 horizontal resolution. 54 vertical levels. Spun up for 50 years
followed by a 57-yr hindcast run (1950–2006). Forcing from the NCEP–NCAR reanalysis.
Time-Mean Volume and Temperature Transport
Results based on XBT measurements at nominal 35S: Total volume transport: 0.5 Sv Total heat transport: 0.54 PW AMOC strength: 17.9 Sv
AMOC from OFES: 15 Sv
Relationship between AMOC and Northward Heat Transport at 35S
HT(PW) 0.05 * AMOC (Sv)
XBT observationsOFES Model
The Strength of the AMOC at 35S
Linear increasing trend in AMOC: 0.9 Sv per decade
Northward Temperature Transport across 35S - I
0.03 PW per decade
Northward Temperature Transport across 35S - III
),()(),( zxvzvvzxv ),()(),( zxzzx
Baroclinic: , Horizontal: )()( zzvcp ),(),( zxzxvcp
Volume Transports across Drake Passage and South of Africa
Temperature Transports across Drake Passage and South of Africa
0.03 PW/decade
-0.04 PW/decade
AfricaDrakeS HTHTQthc
HT 35
0.03 0.03 -0.04Linear Trend (PW/decade)
0.07 PW per decade
Anomalous Air-Sea Heat Flux
Decreasing trend: -0.03 PW/decade
AfricaDrakeS HTHTQthc
HT 35
0.03 -0.3 0.07Linear Trend (PW/decade)
Temperature Transports--- South of Africa
Total-0.04 PW per decade
ACC-dominant eastward transport
0.03 PW per decade
Agulhas leakage-0.07 PW per decade
AgulhasACCAfricaDrakeS HTHTHTQthc
HT ,35
0.03 -0.3 0.03 0.3 0.7Trend
PW/decade
Conclusions Both XBT measurements and the OFES model suggest that 1 sverdrup increase in the AMOC strength would cause an increase in the northward heat transport of 0.05 PW at approximately 35S.
The OFES model suggests an increase in the northward heat transport across 35S from 1980 to 2006.
The increasing trend in the northward heat transport is likely due to the increase in Agulhas leakage into the South Atlantic.
About half of the increase in Agulhas leakage is lost to the atmosphere through air-sea heat exchange.
Temperature Transports across Drake Passage and South of Africa
Northward Temperature Transport across 35S - II