An Improvement on Assimilation of Satellite-derived Sea Surface Temperature for NEMOVAR with the use of MODIS data
- Alternative Title
- MODIS 자료를 활용한 NEMOVAR의 위성 SST 자료동화 개선
- Abstract
- SST is important in coupling the ocean and atmosphere through exchanges of heat, momentum, moisture, and gases. SST data plays a major role as a bottom boundary condition in numerical weather prediction (NWP) systems. Although in-situ measurements are considered to be true values, they have temporal and spatial constraints. A crucial issue is how to implement satellite-derived SST data as boundary conditions for ocean models as well as NWP models.
The operational administrations and organizations have conducted the system for real time global SST products. But, the retrieving high quality and operational ocean initial SST data is still challenging subject. The objective of this thesis is to implement satellite-derived SST measurements into an ocean data assimilation system to improve the ocean-state forecasts.
The Global Ocean Data Assimilation Experiment High-Resolution SST Pilot Project (GHRSST-PP) is a well-organized system providing the near-operational high-resolution satellite SST GHRSST Level 2 Pre-processed data used in this thesis. Advanced Along-track Scanning Radiometer, Advanced Microwave Scanning Radiometer-EOS, Advanced High-Resolution Radiometer, and Moderate Resolution Imaging Spectrometer (MODIS) data are collected and assimilated on the NEMOVAR ocean data assimilation system. The selected datasets have different characteristics and can yield a good effect when used together.
According to the hindcast results, most SST satellite data are well processed. Their RMSEs are less than 0.76°C globally in all seasons (summer, autumn, and winter). However, the RMSEs for SST data from all instruments other than MODIS are approximately 0.5°C globally, even in the summer.
Improving the impact of MODIS on the global dataset will require additional statistics or a quality control (QC) method. A multiple assimilation method based on a variational quality control (VarQC) is proposed. The impacts of additional QC predict that RMSEs will be reduced to less than 40% (average, maximum is 57.45% in Agulhas Return region in June). This type of approach has the advantage of using the scheme itself for quality control. This method can advance the application of satellite data to assimilation systems.
Incidentally, sensitivities to spatial density of GHRSST are acceptable in that the resolution of the satellite-derived SST is close to the model grid rather than denser than the model grid.
- Author(s)
- Mo-Rang Huh
- Issued Date
- 2013
- Awarded Date
- 2013. 8
- Type
- Dissertation
- Publisher
- 부경대학교
- URI
- https://repository.pknu.ac.kr:8443/handle/2021.oak/25356
http://pknu.dcollection.net/jsp/common/DcLoOrgPer.jsp?sItemId=000001966429
- Alternative Author(s)
- 허모랑
- Affiliation
- 대학원
- Department
- 대학원 환경대기과학과
- Advisor
- 오재호
- Table Of Contents
- CONTENTS
Contents ⅰ
List of Tables ⅴ
List of Figures ⅶ
Abstract (English) ⅹⅱ
Abstract (Korean) ⅹⅴ
Chapter 1. Introduction 1
1.1. Overview of general research on satellite-derived SST 2
1.1.1 Operational sea surface temperature from initial ocean data 3
1.2. Objectives 7
Chapter 2. Ocean Data Assimilation System of NEMOVAR 8
2.1. Introduction 8
2.2. General formulation 10
2.2.1. NEMOVAR, a three-dimensional variational data assimilation method
10
2.2.2. Balance operator for ocean state variables 11
2.3. Ocean forecast model of NEMO 14
2.3.1. Model configuration 14
2.3.2. Hindcast results of preceding research 18
2.4 SST bias correction scheme 20
Chapter 3. Observational data 23
3.1. Satellite-derived SST 23
3.1.1. Blending SST data from different sources 28
3.2. Features of satellite SST 33
3.2.1. Advanced Along Track Scanning Radiometer (AATSR) 33
3.2.2. Advanced Microwave Scanning Radiometer-EOS (AMSR-E) 34
3.2.3. Advanced Very High Resolution Radiometer (AVHRR) 36
3.2.4. Moderate Resolution Imaging Spectrometer (MODIS) 37
Chapter 4. Implementation of Satellite SST 40
4.1. Hindcast Experiments 40
4.1.1. Ocean Data 40
4.1.2. Model configurations 42
4.1.3. Experimental design 43
4.1.4. Assessment methods 45
4.2. Subsampling satellite-derived SST 50
4.2.1. Subsampling strategy 50
4.2.2. Confidence flags 52
4.2.3. Subsampling results 54
4.3. Hindcast results 58
4.3.1. SST bias corrections 58
4.3.2. Sensitivity to spatial density 61
4.3.3. Analysis of Innovations 66
Chapter 5. Variational Quality Control for MODIS data 73
5.1. Variational Quality Control 73
5.1.1. Theoretical review 73
5.1.2. Background check method 78
5.1.3. Quality control experimental design 79
5.2. Results of Quality Control Experiment 81
5.2.1. Replacement in AQC 81
5.2.2. Impact of AQC 91
Chapter 6. Summary and Conclusions 95
References 98
Acknowledgements 107
APPENDIX A. The definition of SST 109
APPENDIX B. Vertical grid of NEMO 111
APPENDIX C. CICE: the Los Alamos Sea Ice Model 112
APPENDIX D. Statistics of SST (CTNL) 114
APPENDIX E. Directory of Acronyms (AQC) 120
APPENDIX F. Directory of Acronyms 122
- Degree
- Doctor
-
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