| | [No title] (Site not responding. Last check: 2007-10-21) |
 | | Local time of coverage was also different: for ascending node orbits the Northern Hemisphere was observed in the morning and the Southern Hemisphere in the afternoon, while for descending node orbits the Northern Hemisphere was observed in the afternoon and the Southern in the morning. |
 | | These differences appeared to compensate across the scan, however, an increase in sun glint in descending node over that in ascending node on the western part of the scan was compensated by a decrease on the eastern part of the scan. |
 | | For ascending node, afternoon orbits produced the lowest mean solar zenith angles in the Northern Hemisphere; and morning orbits produced the lowest angles for the Southern Hemisphere. |
| seadas.gsfc.nasa.gov /SeaWiFS/TECH_REPORTS/vol2_abs.html (369 words) |