Print Email Facebook Twitter Early Warning Signals for Regime Transition in the Stable Boundary Layer Title Early Warning Signals for Regime Transition in the Stable Boundary Layer: A Model Study Author van Hooijdonk, I.G.S. (Eindhoven University of Technology) Moene, A. F. (Wageningen University & Research) Scheffer, M. (Wageningen University & Research) Clercx, H. J H (Eindhoven University of Technology) van de Wiel, B.J.H. (TU Delft Atmospheric Remote Sensing) Date 2017-02-01 Abstract The evening transition is investigated in an idealized model for the nocturnal boundary layer. From earlier studies it is known that the nocturnal boundary layer may manifest itself in two distinct regimes, depending on the ambient synoptic conditions: strong-wind or overcast conditions typically lead to weakly stable, turbulent nights; clear-sky and weak-wind conditions, on the other hand, lead to very stable, weakly turbulent conditions. Previously, the dynamical behaviour near the transition between these regimes was investigated in an idealized setting, relying on Monin–Obukhov (MO) similarity to describe turbulent transport. Here, we investigate a similar set-up, using direct numerical simulation; in contrast to MO-based models, this type of simulation does not need to rely on turbulence closure assumptions. We show that previous predictions are verified, but now independent of turbulence parametrizations. Also, it appears that a regime shift to the very stable state is signaled in advance by specific changes in the dynamics of the turbulent boundary layer. Here, we show how these changes may be used to infer a quantitative estimate of the transition point from the weakly stable boundary layer to the very stable boundary layer. In addition, it is shown that the idealized, nocturnal boundary-layer system shares important similarities with generic non-linear dynamical systems that exhibit critical transitions. Therefore, the presence of other, generic early warning signals is tested as well. Indeed, indications are found that such signals are present in stably stratified turbulent flows. Subject Critical regime transitionEarly warning signalsMaximum sustainable heat fluxMinimum wind speedNocturnal boundary layer To reference this document use: http://resolver.tudelft.nl/uuid:66ff62ce-0213-40e0-8d13-61aed4bf0fad DOI https://doi.org/10.1007/s10546-016-0199-9 ISSN 0006-8314 Source Boundary-Layer Meteorology: an international journal of physical and biological processes in the atmospheric boundary layer, 162 (2), 283-306 Part of collection Institutional Repository Document type journal article Rights © 2017 I.G.S. van Hooijdonk, A. F. Moene, M. Scheffer, H. J H Clercx, B.J.H. van de Wiel Files PDF art_3A10.1007_2Fs10546_01 ... 0199_9.pdf 2.04 MB Close viewer /islandora/object/uuid:66ff62ce-0213-40e0-8d13-61aed4bf0fad/datastream/OBJ/view