A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST

Zenghong Liu; Xingrong Chen; Chaohui Sun; Xiaofen Wu; Shaolei Lu

doi:10.1007/s00343-017-5330-3

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A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST

OriginalPaper | Updated：2023-05-16

- A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST
- A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST
- 海洋湖沼学报（英文） 2017年35卷第3期页码：712-721
- Affiliations：
  
  1. State Key Laboratory of Satellite Ocean Environment Dynamics Second Institute of Oceanography State Oceanic Administration
  2. Second Institute of Oceanography State Oceanic Administration
  3. National Marine Environmental Forecasting Center
- Author bio：
- Funds：
  
  Supported by the National Basic Research Program of China (973 Program) (No. 2013CB430301), the National Natural Science Foundation of China (Nos. 41321004, 41206022, 41406022), and the National Special Research Fund for Non-Profit Marine Sector (No. 201305032)
- DOI：10.1007/s00343-017-5330-3
  中图分类号：
- 网络首发：2016-06-29，
  
  纸质出版：2017
- Accepted：
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A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST[J]. 海洋湖沼学报（英文）, 2017,35(3):712-721.

Liu, Z., Chen, X., Sun, C. et al. A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST., Chin. J. Ocean. Limnol. 35, 712–721 (2017). https://doi.org/10.1007/s00343-017-5330-3
A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST[J]. 海洋湖沼学报（英文）, 2017,35(3):712-721. DOI： 10.1007/s00343-017-5330-3.

Liu, Z., Chen, X., Sun, C. et al. A comparison of Argo nominal surface and near-surface temperature for validation of AMSR-E SST., Chin. J. Ocean. Limnol. 35, 712–721 (2017). https://doi.org/10.1007/s00343-017-5330-3 DOI：

摘要

Abstract

Satellite SST (sea surface temperature) from the Advanced Microwave Scanning Radiometer for the Earth Observing System (AMSR-E) is compared with in situ temperature observations from Argo profiling floats over the global oceans to evaluate the advantages of Argo NST (near-surface temperature: water temperature less than 1 m from the surface). By comparing Argo nominal surface temperature (~5 m) with its NST

a diurnal cycle caused by daytime warming and nighttime cooling was found

along with a maximum warming of 0.08±0.36°C during 14:00–15:00 local time. Further comparisons between Argo 5-m temperature/Argo NST and AMSR-E SST retrievals related to wind speed

columnar water vapor

and columnar cloud water indicate warming biases at low wind speed (<5 m/s) and columnar water vapor >28 mm during daytime. The warming tendency is more remarkable for AMSR-E SST/Argo 5-m temperature compared with AMSR-E SST/Argo NST

owing to the effect of diurnal warming. This effect of diurnal warming events should be excluded before validation for microwave SST retrievals. Both AMSR-E nighttime SST/Argo 5-m temperature and nighttime SST/Argo NST show generally good agreement

independent of wind speed and columnar water vapor. From our analysis

Argo NST data demonstrated their advantages for validation of satellite-retrieved SST.

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references

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