engleski

Some recent advances in modeling stable atmospheric boundary layers

The atmospheric boundary layer (ABL) is the lowest part of the atmosphere that is continuously under the influence of the underlying surfaces through mechanical (roughness and shear) and thermal effects (cooling and warming), and the overlying, more free layers. Such boundary layers and the related geophysical turbulence exist also in oceans, seas, lakes and rivers. Here we focus on those in the atmosphere ; however, similar reasoning as presented here also applies to the other geophysical flows mentioned. Since most of human activities and overall life take place in the ABL, it is easy to grasp the need for an ever better understanding of the ABL: its nature, state and future evolution. In order to provide a reasonable and reliable short- or medium-range weather forecast, a decent climate scenario, or an applied micrometeorological study (for e.g. agriculture, road construction, forestry, traffic), etc., the state of the ABL and its turbulence should be properly characterized and marched forward in time in concert with the other prognostic fields. This is one of many tasks of numerical weather prediction and climate models. Many of these models have problems in handling rapid surface cooling under weak or without synoptic forcing (e.g. calm nighttime mountainous or even hilly conditions). Overall research during the last ~ 10 years or so, strongly suggests that the evolution of the stable ABL is still poorly understood today. There we make a contribution by assessing some recent advances in the understanding of nature, theory and modeling of the stable ABL (SABL). In particular, we address inclined very (or strongly) stratified SABL in more details. We show that a relatively thin and very SABL, as recently modeled using an improved "z-less" mixing length scale, can be successfully treated nowadays ; the result is quietly extended to other types of the SABL. Finally, a new generalized "z-less" mixing length- scale is proposed. At the same time, no major improvements in modeling weak-wind strongly-stable ABL is reported yet.

convective ABL; mixing length-scale; Monin-Obukhov length; numerical modeling; parameterization; Prandtl number; Richardson number(s); stratified turbulence; "z-less" turbulence; very stable boundary layer.

Osim projekta BORA, rad se citira i na međunarodnom projektu EMEP4HR (175183/S30).