Freshwater flux (FWF)-induced oceanic feedback in a hybrid coupled model of the tropical Pacific

IOCAS-IR > 海洋环流与波动重点实验室

	Freshwater flux (FWF)-induced oceanic feedback in a hybrid coupled model of the tropical Pacific
	Zhang Ronghua; Busalacchi Antonio J.
	2009-02-15
发表期刊	JOURNAL OF CLIMATE
卷号	22 期号:4 页码:853-879
摘要	The impacts of freshwater flux (FWF) forcing on interannual variability in the tropical Pacific climate system are investigated using a hybrid coupled model (HCM), constructed from an oceanic general circulation model (OGCM) and a simplified atmospheric model, whose forcing fields to the ocean consist of three components. Interannual anomalies of wind stress and precipitation minus evaporation, (P 2 E), are calculated respectively by their statistical feedback models that are constructed from a singular value decomposition (SVD) analysis of their historical data. Heat flux is calculated using an advective atmospheric mixed layer (AML) model. The constructed HCM can well reproduce interannual variability associated with ENSO in the tropical Pacific. HCM experiments are performed with varying strengths of anomalous FWF forcing. It is demonstrated that FWF can have a significant modulating impact on interannual variability. The buoyancy flux (Q(B)) field, an important parameter determining the mixing and entrainment in the equatorial Pacific, is analyzed to illustrate the compensating role played by its two contributing parts: one is related to heat flux (Q(T)) and the other to freshwater flux (Q(S)). A positive feedback is identified between FWF and SST as follows: SST anomalies, generated by El Nino, nonlocally induce large anomalous FWF variability over the western and central regions, which directly influences sea surface salinity (SSS) and Q(B), leading to changes in the mixed layer depth (MLD), the upper-ocean stability, and the mixing and the entrainment of subsurface waters. These oceanic processes act to enhance the SST anomalies, which in turn feedback to the atmosphere in a coupled ocean-atmosphere system. As a result, taking into account anomalous FWF forcing in the HCM leads to an enhanced interannual variability and ENSO cycles. It is further shown that FWF forcing is playing a different role from heat flux forcing, with the former acting to drive a change in SST while the latter represents a passive response to the SST change. This HCM-based modeling study presents clear evidence for the role of FWF forcing in modulating interannual variability in the tropical Pacific. The significance and implications of these results are further discussed for physical understanding and model improvements of interannual variability in the tropical Pacific ocean-atmosphere system.
关键词	Nino-southern-oscillation General-circulation Model Sea-surface Temperature Mixed-layer Model El-nino Equatorial Pacific Interannual Variability Barrier-layer Atmosphere Response Toga Decade
收录类别	SCI
语种	英语
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/18180
专题	海洋环流与波动重点实验室
推荐引用方式 GB/T 7714	Zhang Ronghua,Busalacchi Antonio J.. Freshwater flux (FWF)-induced oceanic feedback in a hybrid coupled model of the tropical Pacific[J]. JOURNAL OF CLIMATE,2009,22(4):853-879.
APA	Zhang Ronghua,&Busalacchi Antonio J..(2009).Freshwater flux (FWF)-induced oceanic feedback in a hybrid coupled model of the tropical Pacific.JOURNAL OF CLIMATE,22(4),853-879.
MLA	Zhang Ronghua,et al."Freshwater flux (FWF)-induced oceanic feedback in a hybrid coupled model of the tropical Pacific".JOURNAL OF CLIMATE 22.4(2009):853-879.

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