Results 251 to 260 of about 759,108 (306)
Some of the next articles are maybe not open access.
2010
This is a book about satellite oceanography and so this chapter about satellite-based measurements of wind and phenomena related to the wind does not attempt to address the topic from the meteorologist’s point of view. For that there are texts devoted to satellite meteorology (e.g., Kidder and Vonder Haar, 1995).
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This is a book about satellite oceanography and so this chapter about satellite-based measurements of wind and phenomena related to the wind does not attempt to address the topic from the meteorologist’s point of view. For that there are texts devoted to satellite meteorology (e.g., Kidder and Vonder Haar, 1995).
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2022
This thesis was scanned from the print manuscript for digital preservation and is copyright the author. Researchers can access this thesis by asking their local university, institution or public library to make a request on their behalf. Monash staff and postgraduate students can use the link in the References field.
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This thesis was scanned from the print manuscript for digital preservation and is copyright the author. Researchers can access this thesis by asking their local university, institution or public library to make a request on their behalf. Monash staff and postgraduate students can use the link in the References field.
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SEA applications to wind instruments
The Journal of the Acoustical Society of America, 2003The behavior of wind instruments, including brass instruments, is primarily determined by the shapes of their air columns, and their interaction with the sound generation mechanism. However, the influence of the surrounding body of the instrument has been a matter of some debate, and papers exploring this question have been published since the early ...
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2020
WNYC-FM Chamber Music Time. Yvette Rudin, violinist; Ada Kopetz, piano.
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WNYC-FM Chamber Music Time. Yvette Rudin, violinist; Ada Kopetz, piano.
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1985
Rivers are channelized flows of water which drain from the continents the precipitation falling as rain or snow, together with the dissolved and entrained particulate products of rock weathering. Today rivers carry annually to the oceans and seas approximately 14 km3 of weathered material, a substantial proportion of it in solution.
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Rivers are channelized flows of water which drain from the continents the precipitation falling as rain or snow, together with the dissolved and entrained particulate products of rock weathering. Today rivers carry annually to the oceans and seas approximately 14 km3 of weathered material, a substantial proportion of it in solution.
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Water Resources, 2001
Analysis of currents in the Caspian and Black seas is made to show that the role of wind-induced currents in the dynamics of seas is largely overestimated and the conventional methods used to evaluate current velocities based on wind speed yield values higher than those observed in the field.
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Analysis of currents in the Caspian and Black seas is made to show that the role of wind-induced currents in the dynamics of seas is largely overestimated and the conventional methods used to evaluate current velocities based on wind speed yield values higher than those observed in the field.
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2002
Abstract The scramble for African possessions among European colonial powers followed a competitive logic that overtook previous rationalizations of colonial- ism, such as the generation of growth in Third World dependencies or the protection of weak client states.
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Abstract The scramble for African possessions among European colonial powers followed a competitive logic that overtook previous rationalizations of colonial- ism, such as the generation of growth in Third World dependencies or the protection of weak client states.
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Expert elicitation survey predicts 37% to 49% declines in wind energy costs by 2050
Nature Energy, 2021Ryan Wiser, Joseph Rand, Joachim Seel
exaly
Quarterly Journal of the Royal Meteorological Society, 1943
AbstractA comparison between theory and observation is made for he problem of veer of wind with height over the sea. Observations made in H.M.ships, notably aircraft carriers, which may be assumed to be at least as accurate as shore based observations are included.
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AbstractA comparison between theory and observation is made for he problem of veer of wind with height over the sea. Observations made in H.M.ships, notably aircraft carriers, which may be assumed to be at least as accurate as shore based observations are included.
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