Abstract

The performance of an atmospheric single-column model (SCM) is studied systematically for stably-stratified conditions. To this end, 11 years (2005–2015) of daily SCM simulations were compared to observations from the Cabauw observatory, The Netherlands. Each individual clear-sky night was classified in terms of the ambient geostrophic wind speed with a 1hbox { m} hbox { s}^{-1} bin-width. Nights with overcast conditions were filtered out by selecting only those nights with an average net radiation of less than -,30hbox { W }hbox {m}^{-2}. A similar procedure was applied to the observational dataset. A comparison of observed and modelled ensemble-averaged profiles of wind speed and potential temperature and time series of turbulent fluxes showed that the model represents the dynamics of the nocturnal boundary layer (NBL) at Cabauw very well for a broad range of mechanical forcing conditions. No obvious difference in model performance was found between near-neutral and strongly-stratified conditions. Furthermore, observed NBL regime transitions are represented in a natural way. The reference model version performs much better than a model version that applies excessive vertical mixing as is done in several (global) operational models. Model sensitivity runs showed that for weak-wind conditions the inversion strength depends much more on details of the land-atmosphere coupling than on the turbulent mixing. The presented results indicate that in principle the physical parametrizations of large-scale atmospheric models are sufficiently equipped for modelling stably-stratified conditions for a wide range of forcing conditions.

Highlights

  • This study investigates to what extent a single-column model (SCM) that is derived from a well-known numerical weather prediction (NWP) model reproduces observed dynamics of the nocturnal boundary layer (NBL) for a wide range of mechanical forcing conditions

  • We explore to what extent the model reproduces qualitatively different NBL regimes that have been distinguished in observations (Sect. 4.2)

  • The present work systematically evaluates the performance of an atmospheric single-column model (SCM) for stably-stratified conditions

Read more

Summary

Introduction

This study investigates to what extent a single-column model (SCM) that is derived from a well-known numerical weather prediction (NWP) model reproduces observed dynamics of the nocturnal boundary layer (NBL) for a wide range of mechanical forcing conditions. To this end, 11 years of daily SCM simulations are compared with observations from the Cabauw observatory in the Netherlands. For each class of geostrophic wind speed, ensemble-averaged profiles and time series of relevant quantities are constructed As such, this approach provides a detailed picture of the model’s performance for a broad range of stabilities, ranging from near-neutral to strongly-stratified conditions. Such a systematic model evaluation is of particular relevance, since the representation of stably-stratified conditions in NWP models is a longstanding challenge in meteorology (e.g. Viterbo et al 1999; Brown et al 2008; Fernando and Weil 2010; Holtslag et al 2013; Sandu et al 2013)

Objectives
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call