| A NOPP Partnership for Skin Sea-Surface Temperature |
2006 |
7 pages |
| Authors:
Peter J. Minnett; R. M. Reynolds; Frank J. Wentz; Andrew T. Jessup; William J. Emery; Gary A. Wick; James A. Cummings; Doug May; ROSENSTIEL SCHOOL OF MARINE AND ATMOSPHERIC SCIENCE MIAMI FL DIV OF METEOROLOGY AND PHYSICAL OCEANOGRAPHY
|
 | As a result of the heat flow between the ocean and overlying atmosphere, the surface of the ocean is nearly always somewhat cooler than the water at a depth of a millimeter or more. The temperature difference across the thermal conductive layer at the sea surface is called the thermal skin effect. During the day, solar heating may cause vertical temperature gradient in the uppermost several meters of the ocean, ... |
|
| Remote Sensing and Modeling of Wildfires |
25 JUL 2005 |
5 pages |
| Authors:
Michele A. Kuester; John Marshall; William J. Emery; BALL AEROSPACE AND TECHNOLOGIES CORP BOULDER CO
|
| The application of satellite remote sensing to the detection and study of wildfires has grown rapidly in recent years as new tools have become available and are put into use. Spaceborne imagery can provide a unique perspective to viewing the fire, giving space/time coverage not available with any other observational system. One aspect of fires that can both be detected with satellite imagery and modeled numerically is the smoke plume ... |
|
| A NOPP Partnership for Skin Sea-Surface Temperature |
2005 |
7 pages |
| Authors:
Peter J. Minnett; R. M. Reynolds; Frank J. Wentz; Andrew T. Jessup; William J. Emery; Gary A. Wick; James A. Cummings; Doug May; ROSENSTIEL SCHOOL OF MARINE AND ATMOSPHERIC SCIENCE MIAMI FL DIV OF METEOROLOGY AND PHYSICAL OCEANOGRAPHY
|
| As a result of the heat flow between the ocean and overlying atmosphere, the surface of the ocean is nearly always somewhat cooler than the water at a depth of a millimeter or more. The temperature difference across the thermal conductive layer at the sea surface is called the thermal skin effect. During the day, solar heating may cause vertical temperature gradient in the uppermost several meters of the ocean, ... |
|
| A NOPP Partnership for Skin Sea-Surface Temperature |
2004 |
7 pages |
| Authors:
Peter J. Minnett; R. M. Reynolds; Frank J. Wentz; Andrew T. Jessup; Edward J. Kearns; William J. Emery; Gary A. Wick; James A. Cummings; Doug May; ROSENSTIEL SCHOOL OF MARINE AND ATMOSPHERIC SCIENCE MIAMI FL DIV OF METEOROLOGY AND PHYSICAL OCEANOGRAPHY
|
| As a result of the heat flow between the ocean and overlying atmosphere, the surface of the ocean is nearly always somewhat cooler than the water at a depth of a millimeter or more. The temperature difference across the thermal conductive layer at the sea surface is called the thermal skin effect. During the day, solar heating may cause vertical temperature gradient in the uppermost several meters of the ocean, ... |
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