Extended Reconstructed Sea Surface Temperature Version 4 (ERSST.v4). Part I: Upgrades and Intercomparisons

被引:837
作者
Huang, Boyin [1 ]
Banzon, Viva F. [1 ]
Freeman, Eric [1 ,2 ]
Lawrimore, Jay [1 ]
Liu, Wei [1 ,3 ]
Peterson, Thomas C. [1 ]
Smith, Thomas M. [4 ,5 ]
Thorne, Peter W. [6 ]
Woodruff, Scott D. [1 ,7 ]
Zhang, Huai-Min [1 ]
机构
[1] Natl Climat Ctr, Asheville, NC 28801 USA
[2] STG Inc, Reston, VA USA
[3] Cooperat Inst Climate & Satellites, Raleigh, NC USA
[4] Univ Maryland, NOAA STAR SCSB, College Pk, MD 20742 USA
[5] Univ Maryland, CICS ESSIC, College Pk, MD 20742 USA
[6] Nansen Environm & Remote Sensing Ctr, Bergen, Norway
[7] Univ Colorado, NOAA, Cooperat Inst Res Environm Sci, Boulder, CO 80309 USA
基金
美国海洋和大气管理局;
关键词
SST; UNCERTAINTY;
D O I
10.1175/JCLI-D-14-00006.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The monthly Extended Reconstructed Sea Surface Temperature (ERSST) dataset, available on global 2 degrees x 2 degrees grids, has been revised herein to version 4 (v4) from v3b. Major revisions include updated and substantially more complete input data from the International Comprehensive Ocean Atmosphere Data Set (ICOADS) release 2.5; revised empirical orthogonal teleconnections (EOTs) and EOT acceptance criterion; updated sea surface temperature (SST) quality control procedures; revised SST anomaly (SSTA) evaluation methods; updated bias adjustments of ship SSTs using the Hadley Centre Nighttime Marine Air Temperature dataset version 2 (HadNMAT2); and buoy SST bias adjustment not previously made in v3b. Tests show that the impacts of the revisions to ship SST bias adjustment in ERSST.v4 are dominant among all revisions and updates. The effect is to make SST 0.1 degrees-0.2 degrees C cooler north of 30 degrees S but 0.1 degrees-0.2 degrees C warmer south of 30 degrees S in ERSST.v4 than in ERSST.v3b before 1940. In comparison with the Met Office SST product [the Hadley Centre Sea Surface Temperature dataset, version 3 (HadSST3)], the ship SST bias adjustment in ERSST.v4 is 0.1 degrees-0.2 degrees C cooler in the tropics but 0.1 degrees-0.2 degrees C warmer in the midlatitude oceans both before 1940 and from 1945 to 1970. Comparisons highlight differences in long-term SST trends and SSTA variations at decadal time scales among ERSST.v4, ERSST.v3b, HadSST3, and Centennial Observation-Based Estimates of SST version 2 (COBE-SST2), which is largely associated with the difference of bias adjustments in these SST products. The tests also show that, when compared with v3b, SSTAs in ERSST.v4 can substantially better represent the El Nino/La Nina behavior when observations are sparse before 1940. Comparisons indicate that SSTs in ERSST.v4 are as close to satellite-based observations as other similar SST analyses.
引用
收藏
页码:911 / 930
页数:20
相关论文
共 50 条
[1]  
[Anonymous], 1996, 120 NOAA
[2]  
Banzon V. F., 2010, P OC SPAC VEN 2010 V, P27, DOI [10.2788/8394, DOI 10.2788/8394]
[3]   LOWESS - A PROGRAM FOR SMOOTHING SCATTERPLOTS BY ROBUST LOCALLY WEIGHTED REGRESSION [J].
CLEVELAND, WS .
AMERICAN STATISTICIAN, 1981, 35 (01) :54-54
[4]   GFDL's CM2 global coupled climate models. Part I: Formulation and simulation characteristics [J].
Delworth, TL ;
Broccoli, AJ ;
Rosati, A ;
Stouffer, RJ ;
Balaji, V ;
Beesley, JA ;
Cooke, WF ;
Dixon, KW ;
Dunne, J ;
Dunne, KA ;
Durachta, JW ;
Findell, KL ;
Ginoux, P ;
Gnanadesikan, A ;
Gordon, CT ;
Griffies, SM ;
Gudgel, R ;
Harrison, MJ ;
Held, IM ;
Hemler, RS ;
Horowitz, LW ;
Klein, SA ;
Knutson, TR ;
Kushner, PJ ;
Langenhorst, AR ;
Lee, HC ;
Lin, SJ ;
Lu, J ;
Malyshev, SL ;
Milly, PCD ;
Ramaswamy, V ;
Russell, J ;
Schwarzkopf, MD ;
Shevliakova, E ;
Sirutis, JJ ;
Spelman, MJ ;
Stern, WF ;
Winton, M ;
Wittenberg, AT ;
Wyman, B ;
Zeng, F ;
Zhang, R .
JOURNAL OF CLIMATE, 2006, 19 (05) :643-674
[5]   The Atlantic multidecadal oscillation and its relation to rainfall and river flows in the continental US [J].
Enfield, DB ;
Mestas-Nuñez, AM ;
Trimble, PJ .
GEOPHYSICAL RESEARCH LETTERS, 2001, 28 (10) :2077-2080
[6]  
FOLLAND CK, 1995, Q J ROY METEOR SOC, V121, P319, DOI 10.1002/qj.49712152206
[7]  
Gregg M. C., 2012, B AM METEOROL SOC, V93, pS57
[8]  
Hartmann DL, 2014, CLIMATE CHANGE 2013: THE PHYSICAL SCIENCE BASIS, P159
[9]   Centennial-Scale Sea Surface Temperature Analysis and Its Uncertainty [J].
Hirahara, Shoji ;
Ishii, Masayoshi ;
Fukuda, Yoshikazu .
JOURNAL OF CLIMATE, 2014, 27 (01) :57-75
[10]  
Hurrell JW, 1999, B AM METEOROL SOC, V80, P2661, DOI 10.1175/1520-0477(1999)080<2661:GSSTAM>2.0.CO