@Article{RaczkaHoDuFoAnBoLi:2021:ImCLBi,
author = "Raczka, Brett and Hoar, Timothy J. and Duarte, Henrique Ferro and
Fox, Andrew M. and Anderson, Jeffrey L. and Bowling, David R. and
Lin, John C.",
affiliation = "{University of Utah} and {National Center for Atmospheric
Research} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Joint Center for Satellite Data Assimilation} and {National
Center for Atmospheric Research} and {University of Utah} and
{University of Utah}",
title = "Improving CLM5.0 Biomass and Carbon Exchange Across the Western
United States Using a Data Assimilation System",
journal = "Journal of Advances in Modeling Earth Systems",
year = "2021",
volume = "13",
number = "7",
pages = "e2020MS002421",
month = "July",
keywords = "data assimilation, CLM, land-atmosphere carbon exchange, biomass
stocks, DART, Western United States.",
abstract = "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.",
doi = "10.1029/2020MS002421",
url = "http://dx.doi.org/10.1029/2020MS002421",
issn = "1942-2466",
language = "en",
targetfile = "2020MS002421.pdf",
urlaccessdate = "11 jun. 2024"
}