A11N-0265
Correlations Between Top-of-atmosphere Net Radiation and Ocean Heat Content
Monday, 14 December 2015
Poster Hall (Moscone South)
Shoichi Taguchi, AIST - National Institute of Advanced Industrial Science and Technology, Tsukuba, Japan
Abstract:
The relationships between observed monthly mean top-of-atmosphere net downward radiation flux (R
T), sea surface temperature (SST), and ocean heat content (O
E) were investigated globally and locally, using EBAF Ed2.8 of CERES and ORAS4 of ECMWF. The tendency of anomalies of global mean SST was correlated (0.5) with the global mean R
T with half-month leads. Local correlations were significant (95%) over 40% area of the ice-free ocean, mostly in the middle latitudes, when the tendency of SST leads R
T by a half month, indicating that the change in SST modifies cloud and atmospheric circulation. The tendency of the global sum of O
E above 100 m for trend length of one month has a contemporary correlation (0.7) with the global mean of R
T anomalies in the 12-month running mean time series, while the size of storage exceeds the amount explained by R
T as shwon in the attached Figure which covers the period from March 2000 to December 2014. Variances with time scales longer than one year for O
E and SST dominated in the Eastern Equatorial Pacific, while those of R
T were relatively smaller there. The maximum and minimum O
E tendencies were found in the tropics, while those of R
T were found at off-equatorial latitudes, indicating oceanic and atmospheric processes connect them. The equivalent ocean depth under the influence of inter-annual R
T variations is uncertain due to limited accuracy of the current datasets.