1952
DOI: 10.1007/bf02019402
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Über Größenunterschiede der Meereswellen bei Warm- und Kaltluft

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Cited by 20 publications
(7 citation statements)
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“…For unstable stratification (air colder than the sea), this downward transport is larger and the waves are expected to be higher than for stable stratification. This presumption has for the first time been proven by the analysis of North Atlantic weather ship data by Roll (1952).…”
Section: Introductionmentioning
confidence: 87%
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“…For unstable stratification (air colder than the sea), this downward transport is larger and the waves are expected to be higher than for stable stratification. This presumption has for the first time been proven by the analysis of North Atlantic weather ship data by Roll (1952).…”
Section: Introductionmentioning
confidence: 87%
“…The cumulated frequencies of these wind data have been plotted on a Gumbel paper (a diagram having the double negative logarithm of the cumulated frequency on the y-axis and the wind speed on the x-axis) using 1-m/s bins. This procedure has also been used in Carter (1993) and Panchang et al (1999) and is based on the assumption that the wind speed time series follows a Fisher-Tippett type 1 Fig. 9 As Fig.…”
Section: Estimation Of Extreme Wavesmentioning
confidence: 99%
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“…The phenomenon, however, has not been studied extensively from a scientific point of view. Roll (1952) analyzed data collectedat certain North Atlantic weather ships and found that for the same measured wind speed, the mean wave height was about 20%…”
Section: The Effects Of Atmospheric Stabilitymentioning
confidence: 99%
“…But, in addition, in a storm moving across the Pacific coast into Oregon, Washington, or British Columbia, the fetch of strong northwesterly winds frequently extends as far south as Southern California a day or two after the storm has reached the coast and then cre ates high waves there which, according to TODD and WIEGEL [1952], may be more important than waves of larger amplitudes generated farther at sea. Finally, cold air masses seem to pro duce higher ocean waves than warm air [ROLL, 1952].…”
Section: Fig 6--surface Meteorological Conditions and Amplitudes Of mentioning
confidence: 96%