Journal
JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS
Volume 13, Issue 7, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2020MS002421
Keywords
data assimilation; CLM; land-atmosphere carbon exchange; biomass stocks; DART; Western United States
Categories
Funding
- NASA CMS Program [NNX16AP33G, 80NSSC20K0010]
- National Science Foundation [UUSL0005, UUSL0007]
- U.S. Department of Energy
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The Western United States is heavily influenced by natural lands that are crucial for carbon balance, water quality, and timber reserves, while also being susceptible to forest mortality from various factors. By adjusting simulations and incorporating water limitations, it is possible to improve carbon monitoring and understand the impact of water availability on carbon uptake through photosynthesis.
The Western United States is dominated by natural lands that play a critical role for carbon balance, water quality, and timber reserves. This region is also particularly vulnerable to forest mortality from drought, insect attack, and wildfires, thus requiring constant monitoring to assess ecosystem health. Carbon monitoring techniques are challenged by the complex mountainous terrain, thus there is an opportunity for data assimilation systems that combine land surface models and satellite-derived observations to provide improved carbon monitoring. Here, we use the Data Assimilation Research Testbed to adjust the Community Land Model (CLM5.0) with remotely sensed observations of leaf area and above-ground biomass. The adjusted simulation significantly reduced the above-ground biomass and leaf area, leading to a reduction in both photosynthesis and respiration fluxes. The reduction in the carbon fluxes mostly offset, thus both the adjusted and free simulation projected a weak carbon sink to the land. This result differed from a separate observation-constrained model (FLUXCOM) that projected strong carbon uptake to the land. Simulation diagnostics suggested water limitation had an important influence upon the magnitude and spatial pattern of carbon uptake through photosynthesis. We recommend that additional observations important for water cycling (e.g., snow water equivalent, land surface temperature) be included to improve the veracity of the spatial pattern in carbon uptake. Furthermore, the assimilation system should be enhanced to maximize the number of the simulated state variables that are adjusted, especially those related to the recommended observed quantities including water cycling and soil carbon.
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