Roles of TAO/TRITON and Argo in tropical Pacific observing system: An OSSE study for multiple time scale variability

Author:

Zhu Jieshun12,Vernieres Guillaume3,Sluka Travis3,Flampouris Stylianos4,Kumar Arun1,Mehra Avichal5,Cronin Meghan F.6,Zhang Dongxiao7,Wills Samantha7,Wang Jiande4,Wang Wanqiu1

Affiliation:

1. 1 Climate Prediction Center, NOAA/NWS/NCEP, College Park, Maryland, USA

2. 2 Earth System Science Interdisciplinary Center, University of Maryland, College Park, Maryland, USA

3. 3 Joint Center for Satellite Data Assimilation, NOAA, College Park, Maryland, USA

4. 4 IMSG at NOAA/NWS/NCEP/EMC, College Park, Maryland, USA

5. 5 Environmental Modeling Center, NOAA/NWS/NCEP, College Park, Maryland, USA

6. 6 Pacific Marine Environmental Laboratory, NOAA, Seattle, WA, USA

7. 7 Cooperative Institute for Climate, Ocean, and Ecosystem Studies, University of Washington, Seattle, WA, USA

Abstract

AbstractIn this study, a series of ocean observing system simulation experiments (OSSEs) are conducted in support of the tropical Pacific observing system (TPOS) 2020 Project (TPOS 2020) which was established in 2014, with aims to develop a more sustainable and resilient observing system for the tropical Pacific. The experiments are based on an ocean data assimilation system that is under development at the Joint Center for Satellite Data Assimilation (JCSDA) and the Environmental Modeling Center (EMC)/National Centers for Environmental Prediction (NCEP). The atmospheric forcing and synthetic ocean observations are generated from a nature run, which is based on a modified CFSv2 with a vertical ocean resolution of 1-meter near the ocean surface. To explore the efficacy of TAO/TRITON and Argo observations in TPOS, synthetic ocean temperature and salinity observations were constructed by sampling the nature run following their present distributions. Our experiments include a free run with no “observations” assimilated, and assimilation runs with the TAO/TRITON and Argo synthetic observations assimilated separately or jointly. These experiments were analyzed by comparing their long-term mean states and variabilities at different time scales [i.e., low-frequency (>90 days), intraseasonal (20~90 days), and high-frequency (<20 days)]. It was found that (1) both TAO/TRITON and especially Argo effectively improve the estimation of mean states and low-frequency variations; (2) on the intraseasonal time scale, Argo has more significant improvements than TAO/TRITON (except for regions close to TAO/TRITON sites); (3) on the high-frequency time scale, both TAO/TRITON and Argo have evident deficits (although for TAO/TRITON, limited improvements were present close to TAO/TRITON sites).

Publisher

American Meteorological Society

Subject

Atmospheric Science

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