Death of an ice sheet
Death of an ice sheet
复制标题
冰原的死亡
作者:
D. Lindstrom;D. Macayeal
SIR-Cahoon et a/. 1 illustrate the use of a satellite in mapping grass or forest fires at night. The wavelength band used was 0.4-1.1!-liD, which spans the visible and very near infrared part of the spectrum. The illumination of cities was eliminated by their permanence, fires being of short duration. Only photographic prints, and not the basic digital information, were archived. The satellite used was one of the Defense Meteorological Satellite Program (DMSP) Block 5, with an effective resolution of about 2.7 km. Routine National Oceanic and Atmospheric Administration (NOAA) meteorological satellites seem more suitable in principle for this task, for every part of the Earth is traversed twice every 24 hours, in midday sunshine and at night. The intensity of sunshine is a maximum at 0.5!! ill (corresponding to a temperature of 6,000 K) and the Earth's emission has a maximum at about be 5 or 10 times as strong as red heat. But a flame with an area of only 20x20 m will outshine I km2 of ordinary territory in bright sunshine and will be seen as very bright at night, while urban illumination is11.0!-liD (300 K). These two emission spectra cross over with an intensity of about one-fortieth of the maximum at a wavelength of about 4!-liD, the precise values depending on the emission temperatures and other factors. The satelliteA pass by NOAA-9 at 13.46 GMT. 12 September 1985, as seen by the channel 3 waveband, which is also in a water vapour window. Fires in which surplus straw is being burned on the farms of England after the harvest can be seen. Other, more regular hotspots are also recorded, such as steel works in Dunquerque and Scunthorpe, and flares on North Sea platforms. But urban areas do not show up at night as they would in a visible waveband (see ref. 2).