globalchange  > 气候变化事实与影响
DOI: 10.1175/JCLI-D-15-0865.1
Scopus记录号: 2-s2.0-85010843455
论文题名:
Simulating ENSO SSTAs from TAO/TRITON Winds: The impacts of 20 years of buoy observations in the Pacific waveguide and comparison with reanalysis products
作者: Chiodi A.M.; Harrison D.E.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2017
卷: 30, 期:3
起始页码: 1041
结束页码: 1059
语种: 英语
Scopus关键词: Atmospheric pressure ; Atmospheric temperature ; Atmospheric thermodynamics ; Buoys ; Climate change ; Climatology ; Flow visualization ; Momentum ; Surface waters ; Waveguides ; Wind stress ; Atmosphere-ocean interactions ; Buoy observations ; ENSO ; Ocean model ; Reanalysis ; Oceanography ; air-sea interaction ; buoy system ; climate change ; data assimilation ; El Nino-Southern Oscillation ; momentum ; sea surface temperature ; temperature anomaly ; wind field ; wind stress ; Pacific Ocean ; Pacific Ocean (Tropical)
英文摘要: The fundamental importance of near-equatorial zonal wind stress in the evolution of the tropical Pacific Ocean's seasonal cycle and El Niño-Southern Oscillation (ENSO) events is well known. It has been two decades since the TAO/TRITON buoy array was deployed, in part to provide accurate surface wind observations across the Pacific waveguide. It is timely to revisit the impact of TAO/TRITON winds on our ability to simulate and thereby understand the evolution of sea surface temperature (SST) in this region. This work shows that forced ocean model simulations of SST anomalies (SSTAs) during the periods with a reasonably high buoy data return rate can reproduce the major elements of SSTA variability during ENSO events using a wind stress field computed from TAO/TRITON observations only. This demonstrates that the buoy array usefully fulfills its waveguide-wind-measurement purpose. Comparison of several reanalysis wind fields commonly used in recent ENSO studies with the TAO/TRITON observations reveals substantial biases in the reanalyses that cause substantial errors in the variability and trends of the reanalysis-forced SST simulations. In particular, the negative trend in ERA-Interim is much larger and the NCEP-NCAR Reanalysis-1 and NCEP-DOE Reanalysis-2 variability much less than seen in the TAO/TRITON wind observations. There are also mean biases. Thus, even with the TAO/TRITON observations available for assimilation into these wind products, there remain oceanically important differences. The reanalyses would be much more useful for ENSO and tropical Pacific climate change study if they would more effectively assimilate the TAO/TRITON observations.
资助项目: NOAA, National Oceanic and Atmospheric Administration
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/49812
Appears in Collections:气候变化事实与影响

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作者单位: Joint Institute for the Study of the Ocean and Atmosphere, University of Washington, Seattle, WA, United States; NOAA/Pacific Marine Environmental Laboratory, Seattle, WA, United States

Recommended Citation:
Chiodi A.M.,Harrison D.E.. Simulating ENSO SSTAs from TAO/TRITON Winds: The impacts of 20 years of buoy observations in the Pacific waveguide and comparison with reanalysis products[J]. Journal of Climate,2017-01-01,30(3)
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