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WANG Jichao,ZHANG Jie,YANG Jungang. 2013. The validation of HY-2 altimetermeasurements of a significant wave height based on buoy data. Acta Oceanologica Sinica, 32(11):87-90
The validation of HY-2 altimetermeasurements of a significant wave height based on buoy data
The validation of HY-2 altimetermeasurements of a significant wave height based on buoy data
Received:December 10, 2012  Revised:March 04, 2013
DOI:10.1007/s13131-013-0382-5
Key words:altimeter  buoy  significant wave height  validation  regression analysis
中文关键词:  altimeter  buoy  significant wave height  validation  regression analysis
基金项目:The Special Funds of State Oceanic Administration for Marine Commonweal Research under contract Nos 201105032-1 and 201305032;the Special Project of State Oceanic Administration of Poles Environmental Investigation and Assessment under contract No. CHINARE2012-02-04;the European Space Agency (ESA)-Minister of Science and Technology of the Peoples Republic of China (MOST) Dragon 3 Cooperation Programme under contract No. 10466.
Author NameAffiliationE-mail
WANG Jichao Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
University of Chinese Academy of Sciences, Beijing 100049, China
College of Science, China University of Petroleum, Qingdao 266580, China 
 
ZHANG Jie First Institute of Oceanography, State Oceanic Administration (SOA), Qingdao 266061, China zhangjie@fio.org.cn 
YANG Jungang First Institute of Oceanography, State Oceanic Administration (SOA), Qingdao 266061, China  
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Abstract:
      HY-2 has been launched by China on August 16, 2011 which assembles multi-microwave remote sensing payloads in a body and has the ability of monitoring ocean dynamic environments. The HY-2 satellite data need to be calibrated and validated before being put into use. Based on the in-situ buoys fromthe National Data Buoy Center (NDBC), Ku-band significant wave heights (SWH, hs) of HY-2 altimeter are validated. Eleven months of HY-2 altimeter Level 2 products data are chose from October 1, 2011 to August 29, 2012. Using NDBC 60 buoys yield 902 collocations for HY-2 by adopting collocation criteria of 30 min for temporal window and 50 km for a spatial window. An overall RMS difference of the SWH between HY-2 and buoy data is 0.297 m. A correlation coefficient between these is 0.964. An ordinary least squares (OLS) regression is performed with the buoy data as an independent variable and the altimeter data as a dependent variable. The regression equation of hs is hs(HY-2)=0.891×hs (NDBC)+0.022. In addition, 2016 collocations are matched with temporal window of 30min at the crossing points of HY-2 and Jason-2 orbits. RMS difference of Ku-band SWH between the two data sets is 0.452 m.
中文摘要:
      HY-2 has been launched by China on August 16, 2011 which assembles multi-microwave remote sensing payloads in a body and has the ability of monitoring ocean dynamic environments. The HY-2 satellite data need to be calibrated and validated before being put into use. Based on the in-situ buoys fromthe National Data Buoy Center (NDBC), Ku-band significant wave heights (SWH, hs) of HY-2 altimeter are validated. Eleven months of HY-2 altimeter Level 2 products data are chose from October 1, 2011 to August 29, 2012. Using NDBC 60 buoys yield 902 collocations for HY-2 by adopting collocation criteria of 30 min for temporal window and 50 km for a spatial window. An overall RMS difference of the SWH between HY-2 and buoy data is 0.297 m. A correlation coefficient between these is 0.964. An ordinary least squares (OLS) regression is performed with the buoy data as an independent variable and the altimeter data as a dependent variable. The regression equation of hs is hs(HY-2)=0.891×hs (NDBC)+0.022. In addition, 2016 collocations are matched with temporal window of 30min at the crossing points of HY-2 and Jason-2 orbits. RMS difference of Ku-band SWH between the two data sets is 0.452 m.
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