GC31D-1221
Climate applications for NOAA 1/4° Daily Optimum Interpolation Sea Surface Temperature

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Patria Viva F Banzon1, Gang Liu2,3, Korak Saha4 and Cara Wilson2, (1)NOAA Asheville, Asheville, NC, United States, (2)NOAA, Boulder, CO, United States, (3)Coral Reef Watch Program - NOAA, College Park, MD, United States, (4)National Centers for Environmental Information-NOAA, Silver Spring, MD, United States
Abstract:
Few sea surface temperature (SST) datasets from satellites have the long temporal span needed for climate studies. The NOAA Daily Optimum Interpolation Sea Surface Temperature (DOISST) on a 1/4° grid, produced at National Centers for Environmental Information, is based primarily on SSTs from the Advanced Very High Resolution Radiometer (AVHRR), available from 1981 to the present. AVHRR data can contain biases, particularly when aerosols are present. Over the three decade span, the largest departure of AVHRR SSTs from buoy temperatures occurred during the Mt Pinatubo and El Chichon eruptions. Therefore, in DOISST, AVHRR SSTs are bias-adjusted to match in situ SSTs prior to interpolation. This produces a consistent time series of complete SST fields that is suitable for modelling and investigating local climate phenomena like El Nino or the Pacific warm blob in a long term context. Because many biological processes and animal distributions are temperature dependent, there are also many ecological uses of DOISST (e.g., coral bleaching thermal stress, fish and marine mammal distributions), thereby providing insights into resource management in a changing ocean. The advantages and limitations of using DOISST for different applications will be discussed.