Harnessing big data to rethink land heterogeneity in Earth system models
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Published:2018-06-14
Issue:6
Volume:22
Page:3311-3330
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ISSN:1607-7938
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Container-title:Hydrology and Earth System Sciences
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language:en
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Short-container-title:Hydrol. Earth Syst. Sci.
Author:
Chaney Nathaniel W., Van Huijgevoort Marjolein H. J., Shevliakova Elena, Malyshev SergeyORCID, Milly Paul C. D., Gauthier Paul P. G., Sulman Benjamin N.ORCID
Abstract
Abstract. The continual growth in the availability, detail, and wealth of environmental
data provides an invaluable asset to improve the characterization of land
heterogeneity in Earth system models – a persistent challenge in macroscale
models. However, due to the nature of these data (volume and complexity) and
computational constraints, these data are underused for global applications.
As a proof of concept, this study explores how to effectively and efficiently
harness these data in Earth system models over a 1/4∘
(∼ 25 km) grid cell in the western foothills of the Sierra Nevada in
central California. First, a novel hierarchical multivariate clustering
approach (HMC) is introduced that summarizes the high-dimensional
environmental data space into hydrologically interconnected representative
clusters (i.e., tiles). These tiles and their associated properties are then
used to parameterize the sub-grid heterogeneity of the Geophysical Fluid
Dynamics Laboratory (GFDL) LM4-HB land model. To assess how this clustering
approach impacts the simulated water, energy, and carbon cycles, model
experiments are run using a series of different tile configurations assembled
using HMC. The results over the test domain show that (1) the observed
similarity over the landscape makes it possible to converge on the macroscale
response of the fully distributed model with around 300 sub-grid land model
tiles; (2) assembling the sub-grid tile configuration from available environmental data can have a large impact on the
macroscale states and fluxes of the water, energy, and carbon cycles; for
example, the defined subsurface connections between the tiles lead to a dampening of macroscale extremes;
(3) connecting the fine-scale grid to the model tiles via HMC enables
circumvention of the classic scale discrepancies between the macroscale and
field-scale estimates; this has potentially significant implications for the
evaluation and application of Earth system models.
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
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