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- W2088293232 abstract "The magnitude of the terms in the equation of motion as applied to motions in the upper troposphere at weather-map scale have been investigated by objective statistical procedures. The appropriate large-scale variance of the radiosonde winds has been extracted from the original record by employing the variance spectrum of isobaric height as a guide to the large-scale structure. The objective analysis shows that the departure of the radiosonde wind from the geostrophic wind is larger in the direction of the flow than transverse to the flow, and the ratio of the standard deviation of the geostrophic departure to the mean wind speed has the same magnitude at 500 and 300 mb. The longitudinal and transverse component ratios have the value 0.25 and 0.15, respectively. Under the most favorable circumstance about half the variance of the observed geostrophic departures must either be due to error or be associated with small-scale motions. The remaining variance of the geostrophic departure at large scale provides an estimate of the large-scale accelerations, which has been confirmed by a correlation of the geostrophic departures with the acceleration of the geostrophic wind. The frictional force has been estimated from the systematics of the geostrophic departures, which suggest that the frictional force, at least in the direction transverse to the flow, approaches a value comparable to the large-scale geostrophic departure. The comparison of geostrophic and radiosonde winds also shows that the poleward transport of momentum in central United States is largely accomplished by the ageostrophic component of the wind." @default.
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- W2088293232 date "1968-08-15" @default.
- W2088293232 modified "2023-10-18" @default.
- W2088293232 title "Magnitude of terms in the equation for large-scale atmospheric motions" @default.
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- W2088293232 doi "https://doi.org/10.1029/jb073i016p05045" @default.
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