Zobrazeno 1 - 6
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pro vyhledávání: '"Dorothy M. Koch"'
Publikováno v:
Bulletin of the American Meteorological Society. 103:E2246-E2264
NOAA has launched the Earth Prediction Innovation Center (EPIC) in partnership with the Weather Enterprise (academia, government, and industry) to bring the power of distributed innovation to bear on one of the greatest challenges of our time. EPIC p
Autor:
Michael E. Mann, Dorothy M. Koch
Publikováno v:
Tellus B; Vol 48, No 3 (1996)
7Be (t1/2 = 53 days) is generated by cosmic rays in the upper troposphere and stratosphere, and is a tracer of downward aerosol transport. We apply a singular value decomposition (SVD)-based technique, which simultaneously determines patterns of sign
Autor:
Michael Manga, Dorothy M. Koch
Publikováno v:
Geophysical Research Letters. 23:225-228
Coronae are typically circular features, 100–600 km in diameter, characterized by a deformed annular ring that is often topographically high. The central region may be raised or depressed relative to the ambient elevation. Previous studies have pro
Autor:
Donald L. Koch, Dorothy M. Koch
Publikováno v:
Journal of Fluid Mechanics. 287:251-278
Numerical solutions are derived for a viscous, buoyant drop spreading below a free fluid surface. The drop has zero interfacial tension, and we consider viscosity contrasts 0.1 < λ < 10 with the surrounding fluid half-space. The density contrast bet
Autor:
Michael E. Mann, Dorothy M. Koch
Publikováno v:
Tellus B: Chemical and Physical Meteorology. 48:387
7 Be ( t 1/2 = 53 days) is generated by cosmic rays in the upper troposphere and stratosphere, and is a tracer of downward aerosol transport. We apply a singular value decomposition (SVD)-based technique, which simultaneously determines patterns of s
Autor:
Dorothy M. Koch, Neil M. Ribe
Publikováno v:
Geophysical Research Letters. 16:535-538
We investigate the effect of lateral viscosity variations on surface observables by considering an idealized model problem: the motion of a deformable fluid sphere of radius a, density ρs and viscosity ηs at a depth d beneath the surface of a fluid