Outlier detection in satellite data using spatial coherence

Abstract Satellite data sets often contain outliers (i.e., anomalous values with respect to the surrounding pixels), mostly due to undetected clouds and rain or to atmospheric and land contamination. A methodology to detect outliers in satellite data sets is presented. The approach uses a truncated Empirical Orthogonal Function (EOF) basis. The information rejected by this EOF basis is used to identify suspect data. A proximity test and a local median test are also performed, and a weighted sum of these three tests is used to accurately detect outliers in a data set. Most satellite data undergo automated quality-check analyses. The approach presented exploits the spatial coherence of the geophysical fields, therefore detecting outliers that would otherwise pass such checks. The methodology is applied to infrared sea surface temperature (SST), microwave SST and chlorophyll-a concentration data over different domains, to show the applicability of the technique to a range of variables and temporal and spatial scales. A series of sensitivity tests and validation with independent data are also conducted.

[1]  R. Evans,et al.  Overview of the NOAA/NASA advanced very high resolution radiometer Pathfinder algorithm for sea surface temperature and associated matchup database , 2001 .

[2]  Pablo Santos,et al.  Real-time, high-resolution, space-time analysis of sea surface temperatures from multiple platforms , 2007 .

[3]  Peter J. Minnett,et al.  An overview of MODIS capabilities for ocean science observations , 1998, IEEE Trans. Geosci. Remote. Sens..

[4]  W. Briggs Statistical Methods in the Atmospheric Sciences , 2007 .

[5]  C. Donlon,et al.  Toward Improved Validation of Satellite Sea Surface Skin Temperature Measurements for Climate Research , 2002 .

[6]  Kozo Okamoto,et al.  Assimilation of SSM/I Radiances in the NCEP Global Data Assimilation System , 2006 .

[7]  J. Beckers,et al.  EOF Calculations and Data Filling from Incomplete Oceanographic Datasets , 2003 .

[8]  perbosc Aberdeen, Scotland-UK , 2011 .

[9]  Bruce D. McKenzie,et al.  Operational Processing of Satellite Sea Surface Temperature Retrievals at the Naval Oceanographic Office , 1998 .

[10]  Christopher J. Merchant,et al.  Optimal estimation of sea surface temperature from split-window observations , 2008 .

[11]  J. Beckers,et al.  Reconstruction of incomplete oceanographic data sets using empirical orthogonal functions: application to the Adriatic Sea surface temperature , 2005 .

[12]  C. Donlon,et al.  OSTIA : An operational, high resolution, real time, global sea surface temperature analysis system , 2007, OCEANS 2007 - Europe.

[13]  R. Daley Atmospheric Data Analysis , 1991 .

[14]  F. Bretherton,et al.  Cloud cover from high-resolution scanner data - Detecting and allowing for partially filled fields of view , 1982 .

[15]  M. Filipiak,et al.  Diurnal warm‐layer events in the western Mediterranean and European shelf seas , 2008 .

[16]  Jean-Marie Beckers,et al.  Cloud filling of ocean colour and sea surface temperature remote sensing products over the Southern North Sea by the Data Interpolating Empirical Orthogonal Functions methodology , 2011 .

[17]  Clemens Reimann,et al.  Statistical data analysis explained : applied environmental statics with R , 2008 .

[18]  Alexander Barth,et al.  Conclusions References , 2004 .