1979
DOI: 10.1175/1520-0493(1979)107<0575:tbousi>2.0.co;2
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The Benefits of Using Short-Interval Satellite Images to Derive Winds for Tropical Cyclones

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Cited by 24 publications
(7 citation statements)
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“…The impact of the image interval has been investigated since the very early days of AMV derivation. Schmetz et al (2000) provide a good summary of this work, which considered optimising coverage both around tropical cyclones (e.g., Rodgers et al, 1979) and more generally. For example, it was found that higher temporal resolution is very important for more rapidly evolving low-level cloud tracers (e.g., Shenk, 1991).…”
Section: Developments In the 1980s-1990smentioning
confidence: 99%
“…The impact of the image interval has been investigated since the very early days of AMV derivation. Schmetz et al (2000) provide a good summary of this work, which considered optimising coverage both around tropical cyclones (e.g., Rodgers et al, 1979) and more generally. For example, it was found that higher temporal resolution is very important for more rapidly evolving low-level cloud tracers (e.g., Shenk, 1991).…”
Section: Developments In the 1980s-1990smentioning
confidence: 99%
“…TC cloud structures are typically fast-evolving due to deformation, evaporation, and vertical shear [41], [42], and cloud features are usually too short-lived to be tracked by routine imaging intervals of meteorological satellites (e.g., 30 min). The study in [43] demonstrates the significance and effectiveness of shorter imaging intervals (3-7.5 min) for improving the observation of rapidly changing features in TC cloud images. Obviously, improving AMV spatial and temporal resolution is essential to tracking cloud features in a TC system, especially in the high-speed zone of the eyewall [37], [41], [43], [44].…”
mentioning
confidence: 84%
“…The images may then be received every three minutes rather than each 30 minutes and smaller cloud elements can be followed for 15 minutes to estimate the velocities. Rodgers et al (1978) were able to track about 6-10 times the usual number of clouds in this way, including some low-level cumulus between breaks in the cirrus overcast. This type of data helps fill the gap between the far-environment of the storm and the inner regions, which can only be sensed with aircraft reconnaissance.…”
Section: Initial Fieldsmentioning
confidence: 99%