Journal of Tropical Oceanography ›› 2019, Vol. 38 ›› Issue (5): 1-9.doi: 10.11978/2018142CSTR: 32234.14.2018142

• Marine Hydrography •     Next Articles

Seasonal variability of the Eastern Tropical Pacific Fresh Pool *

Jianwei CHI1,2,Tangdong QU3,4,Ying ZHANY1,2,Ping SHI1,Yan DU1,2()   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, California 90095, USA
    4. Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, State Oceanic Administration, Qingdao 266000, China;
  • Received:2018-12-27 Revised:2019-02-16 Online:2019-09-20 Published:2019-10-09
  • Contact: Yan DU E-mail:duyan@scsio.ac.cn
  • Supported by:
    Strategic Priority Research Program of Chinese Academy of Sciences(XDA19060501);Strategic Priority Research Program of Chinese Academy of Sciences(XDA13010404);State Oceanic Administration of China(GASI-IPOVAI-02);Natural Science Foundation of China(41525019);Natural Science Foundation of China(41506019);Natural Science Foundation of China(41805057);Natural Science Foundation of China(41830538)

Abstract:

Using the observations and a mixed layer salinity budget from an ocean general circulation model, we investigate the seasonal variability of the eastern tropical Pacific freshwater pool (EPFP). The EPFP has significant seasonal variation, which is controlled by the surface forcing (evaporation and precipitation), horizontal advection and subsurface processes. The seasonal changes in EPFP are mainly divided into two phases: expansion and contraction phases. From April to November, the freshwater pool expands to the west and the freshwater volume and area doubles to 2.83×10 5 km 3 and 8.94×10 6 km 2, respectively. The strong precipitation brought by the northward movement of the intertropical convergence zone is the main reason for the expansion of the EPFP: the surface forcing determines the reduction of the mixed layer salinity. From December to March, when the EPFP shrinks, the increasing of the mixed layer salinity is attributed to the weakening of surface freshwater flux and the enhancement of horizontal advection and subsurface processes.

Key words: the eastern tropical Pacific fresh pool, seasonal variability, mixed layer salinity budget

CLC Number: 

  • P732.26