Turbulent flows are characterized by the non-linear cascades of energy and other inviscid
invariants across a huge range of scales, from where they are injected to where they are …

The exchange of heat, momentum, and mass in the atmosphere over mountainous terrain is
controlled by synoptic-scale dynamics, thermally driven mesoscale circulations, and …

First-order turbulence closure schemes continue to be work-horse models for weather and
climate simulations. The turbulent Prandtl number, which represents the dissimilarity …

The development of a unified similarity scaling has so far failed over complex surfaces, as
scaling studies show large deviations from the empirical formulations developed over flat …

Investigation of meteorological measurements along a 45 m tower at Dome C on the high
East Antarctic Plateau revealed two distinct stable boundary layer (SBL) regimes at this …

Atmospheric internal waves (AIWs) in the boundary layer of atmosphere have been studied
experimentally with the use of Halo Photonics pulsed coherent Doppler wind lidar Stream …

The atmospheric boundary layer is particularly challenging to model in conditions of stable
stratification, which can be associated with intermittent or unsteady turbulence. We develop …

The role of the atmospheric boundary layer (ABL) in the atmosphere-climate system is the
exchange of heat, mass, and momentum between “the earth's surface” and the atmosphere …

Abstract The Innovative Strategies for Observations in the Arctic Atmospheric Boundary
Layer Program (ISOBAR) is a research project investigating stable atmospheric boundary …

An experiment to investigate atmospheric turbulence was performed at Concordia station
(Dome C, Antarctica) during winter 2012, finding significant turbulence in a near-surface …