lmbirch89/CTSM: Arctic Boreal CLM
These code changes provide a better simulation of the carbon cycle in the Arctic-Boreal Zone (ABZ). The changes in the code address biases that arise from using largely temperate schemes in the ABZ. These changes can be classified as: (1) phenology onset, (2) phenology offset, (3) daylight scaling,...
Main Authors: | , , , , , , , , , , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Zenodo
2021
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Subjects: | |
Online Access: | https://dx.doi.org/10.5281/zenodo.4706221 https://zenodo.org/record/4706221 |
Summary: | These code changes provide a better simulation of the carbon cycle in the Arctic-Boreal Zone (ABZ). The changes in the code address biases that arise from using largely temperate schemes in the ABZ. These changes can be classified as: (1) phenology onset, (2) phenology offset, (3) daylight scaling, (4) Leuning temperature scaling, (5) initial spring value of Jmax/Vcmax, (6) dynamic stem-to-leaf carbon allocation, (7) realist root-to-leaf carbon allocation. More details on the biases addressed can be found here: https://doi.org/10.5194/gmd-2020-365 |
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