Remote sensing of lake CDOM using noncontemporaneous field data

There are perhaps millions of lakes in Canada, and remote sensing is a crucial tool for making regional estimates of carbon stocks. Estimation using existing platforms has been hampered by both spatial and spectral resolution, but a new generation of sensors promises greatly improved image quality with broad-scale repeat coverage. Nearly all remote sensing studies in aquatic environments include carefully coordinated field campaigns with satellite overpasses, but this greatly limits the number of lakes that can be used in model development. We explored the opportunities and limits for combining high-quality Advanced Land Imager imagery with legacy lake samples to estimate colored dissolved organic matter (CDOM), a lake characteristic of high value in constructing lake carbon budgets. The passage of time produces somewhat greater scatter than in the standard model with timed field campaign, but there is no indication of a bias toward an incorrect model when using field samples from a variety of dates. Because many thousands of older field samples exist for Canadian lakes, existing limnological databases hold considerable value for estimating CDOM from satellite with sensors of sufficient radiometric depth and signal quality. This study reveals a substantial opportunity for creating and refining estimates of fundamental lake parameters in one of the world's great storehouses of aquatic carbon.

[1]  David M. Lodge,et al.  Regional comparisons of watershed determinants of dissolved organic carbon in temperate lakes from the Upper Great Lakes region and selected regions globally , 2003 .

[2]  H. Paerl,et al.  Measurement of water colour using AVIRIS imagery to assess the potential for an operational monitoring capability in the Pamlico Sound Estuary, USA , 2009, International journal of remote sensing.

[3]  Fred L. Collopy,et al.  Error Measures for Generalizing About Forecasting Methods: Empirical Comparisons , 1992 .

[4]  K. Rose,et al.  Modeling dissolved organic carbon in subalpine and alpine lakes with GIS and remote sensing , 2009, Landscape Ecology.

[5]  L. Tranvik,et al.  Role of lakes for organic carbon cycling in the boreal zone , 2004 .

[6]  Vittorio E. Brando,et al.  Satellite hyperspectral remote sensing for estimating estuarine and coastal water quality , 2003, IEEE Trans. Geosci. Remote. Sens..

[7]  Marvin E. Bauer,et al.  Influence of Chlorophyll and Colored Dissolved Organic Matter (CDOM) on Lake Reflectance Spectra: Implications for Measuring Lake Properties by Remote Sensing , 2006 .

[8]  David Doxaran,et al.  Use of reflectance band ratios to estimate suspended and dissolved matter concentrations in estuarine waters , 2005 .

[9]  Yves T. Prairie,et al.  The pCO2 dynamics in lakes in the boreal region of northern Québec, Canada , 2009 .

[10]  Jonathan J. Cole,et al.  Patterns and regulation of dissolved organic carbon: An analysis of 7,500 widely distributed lakes , 2007 .

[11]  R. Vet,et al.  Regional precipitation and surface water chemistry trends in southeastern Canada (1983–1991) , 1995 .

[12]  S. Carpenter,et al.  Carbon and water cycling in lake‐rich landscapes: Landscape connections, lake hydrology, and biogeochemistry , 2007 .

[13]  Tiit Kutser,et al.  Mapping lake CDOM by satellite remote sensing , 2005 .

[14]  B. Markham,et al.  Summary of Current Radiometric Calibration Coefficients for Landsat MSS, TM, ETM+, and EO-1 ALI Sensors , 2009 .

[15]  Jeffrey A. Cardille,et al.  Small lakes dominate a random sample of regional lake characteristics , 2007 .

[16]  S. Carpenter,et al.  Climate change and lakes: Estimating sensitivities of water and carbon budgets , 2009 .

[17]  J. Dupont Québec Lake Survey: I. Statistical assessment of surface water quality , 1992 .

[18]  G. Kesteven,et al.  The Coefficient of Variation , 1946, Nature.

[19]  P. Frazier,et al.  Water body detection and delineation with Landsat TM data. , 2000 .

[20]  H. Hirtle,et al.  The relation between spectral reflectance and dissolved organic carbon in lake water: Kejimkujik National Park, Nova Scotia, Canada , 2003 .

[21]  Stephen G. Ungar,et al.  Overview of the Earth Observing One (EO-1) mission , 2003, IEEE Trans. Geosci. Remote. Sens..

[22]  Charles E. Brown Applied Multivariate Statistics in Geohydrology and Related Sciences , 1998 .

[23]  Ants Erm,et al.  Optical Properties of Dissolved Organic Matter in Finnish and Estonian Lakes , 2003 .

[24]  Tiit Kutser,et al.  Variations in colored dissolved organic matter between boreal lakes studied by satellite remote sensing , 2009 .

[25]  John M. Melack,et al.  Lakes and reservoirs as regulators of carbon cycling and climate , 2009 .

[26]  Zhen‐Gang Ji Lakes and Reservoirs , 2007, Water‐Quality Engineering in Natural Systems.

[27]  P. Giorgio,et al.  Toward a standard method of measuring color in freshwater , 1992 .

[28]  J. Downing,et al.  Plumbing the Global Carbon Cycle: Integrating Inland Waters into the Terrestrial Carbon Budget , 2007, Ecosystems.

[29]  S. Hooker,et al.  Algorithm development and validation for satellite‐derived distributions of DOC and CDOM in the U.S. Middle Atlantic Bight , 2008 .

[30]  Tiit Kutser,et al.  Using Satellite Remote Sensing to Estimate the Colored Dissolved Organic Matter Absorption Coefficient in Lakes , 2005, Ecosystems.

[31]  B. Gentili,et al.  A simple band ratio technique to quantify the colored dissolved and detrital organic material from ocean color remotely sensed data , 2009 .

[32]  J. Downing,et al.  The global abundance and size distribution of lakes, ponds, and impoundments , 2006 .

[33]  John R. Schott,et al.  The increased potential for the Landsat Data Continuity Mission to contribute to case 2 water quality studies , 2009, Optical Engineering + Applications.

[34]  Jonathan J. Cole,et al.  Synchronous variation of dissolved organic carbon and color in lakes , 2002 .

[35]  Julia A. Barsi,et al.  The next Landsat satellite: The Landsat Data Continuity Mission , 2012 .

[36]  D. B. Kleja,et al.  Variation in Organic Matter and Water Color in Lake Mälaren during the Past 70 Years , 2010, AMBIO.

[37]  C. Justice,et al.  Atmospheric correction of MODIS data in the visible to middle infrared: first results , 2002 .