Polar Oceans from Space

Only a few centuries ago, we knew very little about our planet Earth. The Earth was considered flat by many although it was postulated by a few like Aristotle that it is spherical based on observations that included the study of lunar eclipses. Much later, Christopher Columbus successfully sailed to the West to discover the New World and Ferdinand Magellan’s ship circumnavigated the globe to prove once and for all that the Earth is indeed a sphere. Worldwide navigation and explorations that followed made it clear that the Earth is huge and rather impossible to study solely by foot or by water. The advent of air travel made it a lot easier to do exploratory studies and enabled the mapping of the boundaries of continents and the oceans. But aircraft coverage was limited and it was not until the satellite era that full c- erage of the Earth’s surface became available. Many of the early satellites were research satellites and that meant in part the development of engineering measurement systems with no definite applications in mind. The Nimbus-5 Electrically Scanning Microwave Radiometer (ESMR) was a classic case in point. The sensor was built with the idea that it may be useful for meteorological research and especially rainfall studies over the oceans, but success in this area of study was very limited.

Background.- Fundamental Characteristics of the Polar Oceans and Their Sea Ice Cover.- Satellite Remote Sensing Techniques.- Geophysical Parameters and Algorithms for High Latitude Applications.- Variability of Surface Pressure, Winds, and Clouds.- Variability of Surface Temperature and Albedo.- Characteristics and Variability of the Sea Ice Cover.- Polynyas and Other Polar Phenomena.- Variability of Phytoplankton Pigment Concentrations and Primary Productivity.- Decadal Changes, Correlations, and Trends.

Josefino C. Comiso is a Senior Research Scientist of the Oceans and Ice Branch Division of the NASA Goddard Space Flight Center. His current research interests include: (a) the detection of climate change from historical data; (b) the role of Odden and polynyas in ocean convection and bottom water formation; (c) air-sea-ice interactions and biological processes in the polar regions; (d) radiative transfer modelling studies and satellite algorithms for sea, ice and snow.