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Leaf chlorophyll constraint on model simulated gross primary productivity in agricultural systems.

TL;DR: The results support the use of Chll as an observational proxy for V max 25 and future work needs to be directed towards improving the Chll retrieval accuracy from space observations and developing consistent and physically realistic modeling schemes that can be parameterized with acceptable accuracy over spatial and temporal domains.
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A sensitivity study of high-resolution regional climate simulations to three land surface models over the western United States

TL;DR: In this paper, the authors applied the Weather Research Forecasting model for convection-permitting regional climate simulations over the western United States using three different land surface schemes (Noah, NoahMP, and CLM).
Journal ArticleDOI

Evaluation of the New CNDV Option of the Community Land Model: Effects of Dynamic Vegetation and Interactive Nitrogen on CLM4 Means and Variability*

TL;DR: The Community Land Model, version 4 (CLM4) includes the option to run the prognostic carbon-nitrogen (CN) model with dynamic vegetation (CNDV) as mentioned in this paper.
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The Global Gridded Crop Model Intercomparison phase 1 simulation dataset

TL;DR: The Global Gridded Crop Model Intercomparison (GGCMI) phase 1 dataset provides an unprecedentedly large dataset of crop model simulations covering the global ice-free land surface and is aimed at promoting further analyses and understanding of cropmodel performance, potential relationships between productivity and environmental impacts, and insights on how to further improve global gridded crop model frameworks.
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The impact of different glacial boundary conditions on atmospheric dynamics and precipitation in the North Atlantic region

TL;DR: In this article, the impact of different glacial boundary conditions on precipitation and atmospheric dynamics in the North Atlantic region is investigated using a highly resolved atmospheric general circulation model, using six 30-yr time slice experiments of the Last Glacial Maximum at 21 thousand years before the present (ka BP) and of a less pronounced glacial state (65 ka BP) to analyse the sensitivity to changes in the ice sheet distribution, in the radiative forcing and in the prescribed time-varying sea surface temperature and sea ice, which are taken from a lower-resolved, but
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