«UPDRAUGHT»に関連する英語の本
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1
Data Assimilation for Atmospheric, Oceanic and Hydrologic ...
Entrainment and Detrainment Entrainment rate in the updraught (6..) is split into
turbulent and organized components, which are both modulated by humidity
conditions in the environment. Detrainment in the updraught (SL,) is assumed to
...
Seon Ki Park, Liang Xu, 2013
2
Advanced Renewable Energy Sources
(A) Fixed-Bed Gasifier There are three main designs of fixed bed gasifiers
namely (i) updraught (ii) downdraught (iii) crossdraught. (i) Updraught-Type
Gasifier An updraught type gasifier is known as a counterflow gasifier. It is the
simplest as ...
G. N. Tiwari, Rajeev Kumar Mishra, 2011
3
Fundamentals of Weather and Climate
sionally, on the basis of some exceedingly bumpy traverses by military aircraft
and 10.6 Severe local storms dramatic inadvertent ascents by gliders, and from
indirect evidence such as the height of updraught overshoot into the stratosphere
...
updraught low level inflow Figure 3 Diagram of a severe tornadic thunderstorm,
typical of those on the plains in the American Mid West Figure 3 shows the
essential structure of a tornado- bearing thunderstorm, commonly referred to as a
...
7.7 Updraught slope For r = 0, we have I6 = 1, and 2* = H /2 ; the neutrally
stratified flow is turned round, but is otherwise unchanged. For r > 0 the inflow is
convectively buoyant I6 > 1, and 2,, > H /2. Thus the steering level is above the
middle ...
John Green, John Sydney Adcock Green, 1999
6
Recent Progress in Many-Body Theories
The column is divided into successive horizontal layers, typically 100m deep,
with allowance for entrainment of air into the updraught. At each horizontal level
budgets into and out of each layer in the column are maintained for air, vapour, ...
T. L. Ainsworth, B. E. Clements, 1992
7
Air Pollution Modeling and Its Application IX
The column is divided into successive horizontal layers, typically 100m deep,
with allowance for entrainment of air into the updraught. At each horizontal level
budgets into and out of each layer in the column are maintained for air, vapour, ...
Han Dop, H. Van Dop, George Kallos, 1992
8
The Physics and Parameterization of Moist Atmospheric Convection
The closure of the scheme differs from that described above in that only
updraught fluxes of moisture out of the boundary layer are considered to balance
the forcing in the sub-cloud layer. This does not affect the average properties of ...
9
Boundary-Layer Meteorology 25th Anniversary Volume, ...
This is also the reason for the fact that the updraught branch of the cross-frontal
circulation and the SCF is retarded towards the cold side of the jet in the LTJ case
(.r = 100 km in Figure 4c) and is accelerated towards the warm side of the jet in ...
R. E. Munn, John R. Garratt, P.A. Taylor, 1996
10
Interdisciplinary Aspects of Turbulence
A straightforward decomposition of p through Eq. (42) assumes a zero-order
pressure jump across the updraught–downdraught interface that would result in a
spurious source term in the equation for the vertical-velocity variance. A rigorous
...
Wolfgang Hillebrandt, Friedrich Kupka, 2009
