Diurnal variation correction of AVHRR SST data for the Northwest Pacific region

  • TENG Wei-cheng ,
  • GUAN Lei
Expand
  • Ocean Remote Sensing Institute/Department of Marine Technology, College of Information Science and Engineering, Ocean University of China, Qingdao 266100, China

Received date: 2011-01-14

  Revised date: 2011-04-20

  Online published: 2012-10-24

Abstract

There is a near-surface diurnal warming layer due to the effect of solar heating during the daytime. The diurnal variation is important for studying air-sea interaction and marine ecology, among others. The characteristics of the diurnal variation are different in different regions. In this paper, firstly the empirical and physical models for estimating diurnal warming are introduced. Secondly, the sea surface temperature (SST) from the National Oceanic and Atmospheric Administration (NOAA) Advanced Very High Resolution Radiometer (AVHRR), surface wind speed of Aqua Advanced Microwave Scanning Radiometer for EOS (AMSR-E) and solar radiation in the Northwest Pacific are used to regress the coefficients in an empirical model, which is applied in the diurnal variation correction of NOAA AVHRR SST in the studied area. It shows that, for the correction of AVHRR SST, the mean bias is b0.01℃ and the standard deviation is 0.22℃. The new model can be applied in the diurnal variation correction of the satellite data in the Northwest Pacific.

Cite this article

TENG Wei-cheng , GUAN Lei . Diurnal variation correction of AVHRR SST data for the Northwest Pacific region[J]. Journal of Tropical Oceanography, 2012 , 31(4) : 1 -7 . DOI: 10.11978/j.issn.1009-5470.2012.04.001

References


[1] SVERDRUP H U, JOHNSON M W, FLEMING R H. The oceans: Their physics, chemistry and general biology [M]. New York: Prentice-Hall, Englewood Cliffs, 1942: 60–64.
SCHLUESSEL P, EMERY W J, GRASSL H, et al. On the bulk-skin temperature difference and its impact on satellite remote sensing of sea surface temperature [J]. Geophys Res, 1990, 95: 13341–13356.
FAIRALL C W, BRADLEY E F, GODFREY J S, et al. Cool-skin and warm-layer effects on sea surface temperature [J]. Geophys Res, 1996, 101:1295–1308.
DONLON C J, MINNETT P J, GENTEMANN C, et al. Toward improved validation of satellite sea surface skin temperature measurements for climate research [J]. Climate, 2002, 15: 353–369.
WANG SUFEN, TANG DANLING. Remote Sensing of Day/Night Sea Surface Temperature Difference Related to Phytoplankton Blooms [J]. International Journal of Remote Sensing, 2010,31(17-18): 4569-4578
Implementation Advisory Group. Global physical ocean observations for GOOS/GCOS: An action plan for existing bodies and mechanisms [M]. Paris: GOOS Rep 66, Intergov Oceanogr Comm, 1999: 6.
WOODS J D, BARKMANN W, HORCH A. Solar heating of the oceans-diurnal, seasonal, and meridional variations [J]. Quarterly Journal of the Royal Meteorological Society, 1984, 110, 633-686.
WEBSTER P J, CLAYSON C A, CURRY J A. Clouds, radiation, and the diurnal cycle of sea surface temperature in the tropical western Pacific [J]. Climate, 1996, 9:1712–1730.
QIU CHUNHUA, WANG DONGXIAO, KAWAMURA H, et al. Validation of AVHRR and TMI-derived sea surface temperature in the northern South China Sea [J]. Continental Shelf Research, 2009, 29: 2358–2366
PALMER T N, MANSFIELD D A. Response of two atmospheric general circulation models to sea-surface temperature anomalies in the tropical East and West Pacific [J]. Nature, 1984, 310(5977): 483-485.
SHUKLA J. Predictability in the midst of chaos: A scientific basis for climate forecasting [J]. Science, 1998, 282(5389): 728-731.
DONLON C J, MINNETT P J, BARTON I J, et al. The character of skin and subsurface sea surface temperature [R]. Switzerland: World Meteorol Organ, Geneva, 2001: 298-302.
STOMMEL H, SAUNDERS K, SIMMONS W et al. Observations of the diurnal thermocline [J]. Deep-Sea Res, 1969, 16: 269–284.
KAWAI Y, KAWAMURA H. Evaluation of the diurnal warming of sea surface temperature using satellite-derived marine meteoro- logical data [J]. Oceanogr, 2002, 58: 805–814.
GENTEMANN C L, DONLON C J, STUART-MENTETH A, et al. Diurnal signals in satellite sea surface temperature measurements[J]. Geophys Res, 2003, 30(3): 1140.
CLAYSON C A, WEITLICH D. Diurnal warming in the tropical Pacific and its interannual variability [J]. Geophys Res, 2005, 32: L21604.
LIOU, KUO-NAN. An introduction to Atmospheric Radiation[M]. New York: Academic Press Inc, 2002: 45-51.
KAWAI Y, WADA A. Diurnal Sea Surface Temperature Variation and Its Impact on the Atmosphere and Ocean: A Review [J]. Oceanogr, 2007, 63: 721-744.
SOLOVIEV A, LUKAS R. The near-surface layer of the ocean: Structure, dynamics and application [M]. Dordrecht: Atmospheric and Oceanographic Sciences Library, 2006: 496-502.
PRICE J F, WELLER R A, BOWERS C M et al. Diurnal response of sea surface temperature observedat the long-term upper ocean study (34°N, 70°W) in the Sargasso Sea [J]. Geophys Res, 1987, 92: 14480–14490.
KANTHA L H, CLAYSON C A. An improved mixed layer model for geophysical applications [J]. Geophys Res, 1994, 99: 25235–25266.
ALICE C, STUART-MENTETH, ROBINSON I S. A global study of diurnal warming using satellite- derived sea surface temperature [J]. Geophys Res Let, 2003, 108: 3155.
PRICE J F, WELLER R A, PINKEL R. Diurnal cycling: observations and models of the upper ocean response to diurnal heating, cooling and wind mixing [J].Gephys Res 1986, 91: 8411-8427.
GENTEMANN C L, MINNETT P J, WARD B. Profiles of Ocean Heating (POSH): a new model of upper ocean diurnal thermal variability [J]. Geophys Res, 2009, 114: C07017.
LARGE W G, WILLIAMS M, DONEY S C. Ocean vertical mixing: A review and a model with a nonlocal boundary layer parameterization [J]. Rev geophysics, 1994, 32: 363-403.
WARD B, WANNINKHOF R, MCGILLIS W R, et al. Biases in the air-sea flux of CO2 resulting from ocean surface temperature gradients [J]. Geophys Res, 2004, 109: C08S08.
ZENG X, BELJAARS A. A prognostic scheme of sea surface skin temperature for modeling and data assimilation [J]. Geophys Res, 2005, 32: L14605.
Outlines

/