2003
DOI: 10.1029/2002rs002632
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Air temperature profile and air/sea temperature difference measurements by infrared and microwave scanning radiometers

Abstract: [1] A system of two scanning radiometers has been developed by the National Oceanic and Atmospheric Administration/Environmental Technology Laboratory and deployed on the NOAA R/V Ronald H. Brown during the Nauru99 cruise in the tropical western Pacific in June and July 1999. The system is composed of a high-quality temperature sensor and two independent, vertically scanning radiometers, measuring atmospheric and oceanic emission in the microwave (MW), and infrared (IR) regions. Both radiometers measure emissi… Show more

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Cited by 12 publications
(7 citation statements)
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“…(Schwier et al, ). The stability of the MBL can be described approximately by the difference between air temperature ( T A ) and SST; i.e., the MBL is stable when T A ‐SST > 0 and is unstable when T A ‐SST < 0 (Cimini et al, ; R. M. Williams, ). Waves appear to grow more rapidly under unstable conditions (Young, ).…”
Section: Resultsmentioning
confidence: 99%
“…(Schwier et al, ). The stability of the MBL can be described approximately by the difference between air temperature ( T A ) and SST; i.e., the MBL is stable when T A ‐SST > 0 and is unstable when T A ‐SST < 0 (Cimini et al, ; R. M. Williams, ). Waves appear to grow more rapidly under unstable conditions (Young, ).…”
Section: Resultsmentioning
confidence: 99%
“…In fact the air/sea temperature difference generally varies near the zero under the influence of many factors [24][25][26].…”
Section: Off-design Behavior Modelmentioning
confidence: 99%
“…Maximum mean values of AOD are found in deserted arid areas (Sahara, Kalahari, Arabian, Gobi) where a lot of dust is emmited in the atmosphere. Finally, in cases of volcanic eruptions (Stenchikov et al, 2002, Ansmann et al, 2011 and forest fires (Colarco et al, 2004, Stohl et al,2006 corresponding aerosols are emitted in the atmosphere and not include in aerosols climatology, due to their unique and random nature, but result to very high AOD recordings. More recently (Taylor et al, 2015), there has been an approach to characterise atmospheric aerosol mixtures that contain different ratios of particles (figure 2.12).…”
Section: Figure 210 Schematic Visualization Of Absorbing and Scattering Aerosols'mentioning
confidence: 99%
“…Emitting of atmospheric gases at well-defined bandwidths is estimated by microwave radiation received at the surface. Algorithms for retrieving IWV, are based on inversion techniques, which are using retrieved temperature profiles -derived from oxygen emission lines -fitted to model profiles either by neural networks (Churnside et al, 1994), Kalman filtering (Ledskam and Staelin, 1978)…”
Section: Microwave Radiometer Profiler (Mwp)mentioning
confidence: 99%
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