L. M. Mack
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View article: Probabilistic modelling of atmosphere-surface coupling with a copula Bayesian network
Probabilistic modelling of atmosphere-surface coupling with a copula Bayesian network Open
Land-atmosphere coupling is an important process for correctly modelling near-surface temperature profiles, but it involves various uncertainties due to subgrid-scale processes, such as turbulent fluxes or unresolved surface heterogeneitie…
View article: Investigating Stable Boundary-Layer Temperature Profiles Observed from Fiber-Optic Distributed Sensing on a Tethered Balloon and comparing them against NWP Systems at Different Resolutions for an Arctic Fjord-Valley System in Svalbard
Investigating Stable Boundary-Layer Temperature Profiles Observed from Fiber-Optic Distributed Sensing on a Tethered Balloon and comparing them against NWP Systems at Different Resolutions for an Arctic Fjord-Valley System in Svalbard Open
Stable boundary layers (SBL) commonly form during the Arctic polar night, but their correct representation has been posing major challenges for numerical weather prediction (NWP) systems. To enable innovative model verification, we perform…
View article: Stable Boundary Layers in an Arctic Fjord‐Valley System: Evaluation of Temperature Profiles Observed From Fiber‐Optic Distributed Sensing and Comparison to Numerical Weather Prediction Systems at Different Resolutions
Stable Boundary Layers in an Arctic Fjord‐Valley System: Evaluation of Temperature Profiles Observed From Fiber‐Optic Distributed Sensing and Comparison to Numerical Weather Prediction Systems at Different Resolutions Open
Stable boundary layers (SBLs) commonly form during the Arctic polar night, but their correct representation poses a major challenge for numerical weather prediction (NWP) systems. To enable detailed model verification, we performed measure…
View article: Transfer Efficiency and Organization in Turbulent Transport over Alpine Tundra
Transfer Efficiency and Organization in Turbulent Transport over Alpine Tundra Open
The exchange of momentum, heat and trace gases between atmosphere and surface is mainly controlled by turbulent fluxes. Turbulent mixing is usually parametrized using Monin–Obukhov similarity theory (MOST), which was derived for steady tur…
View article: Stable Boundary Layers in an Arctic Fjord-Valley System: Evaluation of Temperature Profiles Observed from Fiber-Optic Distributed Sensing and Comparison to NWP Systems at Different Resolutions
Stable Boundary Layers in an Arctic Fjord-Valley System: Evaluation of Temperature Profiles Observed from Fiber-Optic Distributed Sensing and Comparison to NWP Systems at Different Resolutions Open
Stable boundary layers commonly form during Arctic polar night, but their correct representation poses a major challenge for numerical weather prediction (NWP) systems. To perform detailed model verification by probing the lower boundary l…
View article: Climatologies of Anisotropy in the Reynolds Stress Tensor
Climatologies of Anisotropy in the Reynolds Stress Tensor Open
Turbulent mixing processes in the atmospheric boundary layer are usually described using Monin-Obukhov similarity theory (MOST), which combines the mean flow properties in the dimensionless stability parameter. Originally, this theory was …