Start Date: End Date: Published Date Data Date
Data acquired September 23, 1998 293 x 755 460 KB - PNG
The whiting over Lake Michigan in this SeaWiFS image is probably a result of a calcite whiting that typically occurs as a result of autogenic precipitation of calcite as a result of water warming and a pH rise caused by phytoplankton uptake of carbon dioxide.
Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE
Published September 23, 1998 Data acquired September 23, 1998