Zobrazeno 1 - 10
of 681
pro vyhledávání: '"J. W. Deardorff"'
Autor:
Clayton A. Paulson
Publikováno v:
Journal of Geophysical Research. 74:2141-2142
Autor:
Paulson, Clayton A.
Publikováno v:
Journal of Geophysical Research; 1969, Vol. 74 Issue 8, p2141-2142, 2p
Autor:
Lilly, Douglas K.
Publikováno v:
Journal of the Atmospheric Sciences. 12/1/2002, Vol. 59 Issue 23, p3353. 9p.
Autor:
Li, Ning, Guo, Jianping, Wu, Mengxi, Zhang, Fan, Guo, Xiaoran, Sun, Yuping, Zhang, Zhen, Liang, Hong, Chen, Tianmeng
Publikováno v:
Geophysical Research Letters; 10/28/2024, Vol. 51 Issue 20, p1-10, 10p
Autor:
P. C. Manins, J. W. Deardorff
Publikováno v:
Quarterly Journal of the Royal Meteorological Society. 109:677-681
Autor:
J. W. Deardorff
Publikováno v:
Journal of Applied Meteorology. 16:1182-1185
A rate equation for soil-surface moisture fraction is developed which makes use of the more customary bulk soil moisture content, as well as the soil-surface evaporation rate minus precipitation rate. The two empirical constants involved are estimate
Autor:
J. W. Deardorff, Sergej Zilitinkevich
Publikováno v:
Journal of the Atmospheric Sciences. 31:1449-1452
The conventional similarity theory for the planetary boundary layer is amended to contain the actual boundary-layer height scale h rather than the neutral rotation height scale u*/|f|.
Autor:
Paul H. Ruscher, J. W. Deardorff
Publikováno v:
Tellus A; Vol 34, No 6 (1982)
A mesoscale mixed-layer model of the planetary boundary layer is applied to the flow past a mountain island during a cold air outbreak over the Kuroshio Current. Utilizing data taken during AMTEX '75, the governing equations are integrated in time to
Publikováno v:
Journal of the Atmospheric Sciences. 39:2464-2476
Numerical integrations using a potential enstrophy-conserving scheme are presented for the flow within a mixed layer over hilly terrain using the hydrostatic shallow-water equations with a quadratic drag law. The mesoscale area treated is 150 km on a
Autor:
J. W. Deardorff, E. W. Peterson
Publikováno v:
Journal of the Atmospheric Sciences. 37:1405-1409
A local interfacial boundary condition between a turbulent and non-turbulent layer is constructed in a manner that allows local entrainment. The Reynolds average of this equation produces a mean boundary-layer growth rate that contains additional ter