Numerical modelling of the depth variation and the fluctuation of the thermocline under the effects of wind in the Bohai Sea

-In this paper, numerical modelling of the fluctuation of the thermocline in the Bohai Sea has been made using a two-dimensional nonlinear model in stratified ocean and the model for the depth of the thermocline under the effects of wind stirring. The computed results depict the variations of the fluctuation of the thermocline driven by different kinds of wind fields. The fluctuation of the thermocline in the Bohai Sea varies somewhat with different directions, paths and locations of typhoon (cyclone). Under the effects of strong wind, the thermoclines both sink due to mixing and fluctuate. Furthermore, the fluctuation of the thermocline speeds up mixing. At last, the thermoclines disappear after 12-15 h when the strong wind increases from Force 6 to Force 9.

EFFECTS OF WIND SHEAR ON ATMOSPHERIC GRAVITY WAVE SPECTRUM

The effects of constant wind shear on atmospheric gravity wave spectrum are examined.At first a three- dimensional equilibrium spectral model of gravity waves is established in which wind shear rate β is implicit. Based on this model,the expressions for one-dimensional frequency spectrum of atmospheric gravity waves are derived in which β is explicit.Numerical results show that (1) if we assume that mean wind U(z)=βz (z represents the altitude) and the internal gravity wave spectrum at the altitude of U=0 (that is,z=0) is VanZandt one,then the effect of Doppler shifting due to mean wind may be ignored;(2) when Richardson number J(J=N^2/β~2,N is Brunt-V(?)is(?)l(?) frequency,and is equal to 10^(-2)s^(-1) in this paper) satisfies J≥10.0,the effects ofwind shear arealso ignored;(3)for f^2(?)ω~2(?)N^2 (f is the inertia frequency,and f=10^(-4)s^(-1) in this paper,and co is the observed frequency),the wind shear only affects the spectral amplitude,and does not alter the spectral shape;and (4) as wind shear becomes strong,a part of wave potential energy turns into wave kinetic one,and a part of the vertical kinetic energy further turns into the horizontal one.

A TWO-DIMENSIONAL NUMERICAL STUDY OF WIND SHELTERING EFFECTS OF SHELTERBELTS

Based on the dynamic and thermodynamic equations in the SBL,the protection characteristics and mech- anism of shelterbelts are numerically studied in this paper.The results are in consistent with those ob- served in fields and wind-tunnels.Research shows that the belts with a permeability of 0.3—0.4 have the maximum sheltering effects.The distance where wind speed reduces at least by 20% is at 18—19 times of tree height(H)behind belts.The protection distance reduces fast with the increase of the permeability and slowly with its decrease.The belts have weaker sheltering effects in upstream,generally beyond 6H in front of belts there are no sheltering effects.In addition,the belts with low permeability at top and high permeability at bottom have much better sheltering effects than the belts with high permeability at top and low permeability at bottom.The belts with 50% overall permeability reduce wind speed at least,by 20% at the distance of 5H on the leeward side and by 10% at 11H.When the air is unstable,the protecting effects will be reduced.For the uniform belts with a permeability of 0.35,the distance where wind speed reduces at least by 20% is 15H under the unstable air and 13H under very unstable air.The belts reduce the turbulent diffusion coefficient at the bottom of belts,but increase it at the top.