A Comparison of the Diel Cycle of Modeled and Measured Latent Heat Flux During the Warm Season in a Colorado Subalpine Forest

Burns, Sean P.; Swenson, Sean C.; Wieder, William R.; Lawrence, David M.; Bonan, Gordon B.; Knowles, John F.; Blanken, Peter D.

doi:10.1002/2017MS001248

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The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.

i

A Comparison of the Diel Cycle of Modeled and Measured Latent Heat Flux During the Warm Season in a Colorado Subalpine Forest

2018
By Burns, Sean P. ; Swenson, Sean C. ; Wieder, William R. ; ...
Source: Journal of Advances in Modeling Earth Systems, 10(3), 617-651

[PDF-2.47 MB]

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Journal Title:

Journal of Advances in Modeling Earth Systems
Personal Author:

Burns, Sean P. ; Swenson, Sean C. ; Wieder, William R. ; Lawrence, David M. ; Bonan, Gordon B. ; ... More +

Burns, Sean P. ; Swenson, Sean C. ; Wieder, William R. ; Lawrence, David M. ; Bonan, Gordon B. ; Knowles, John F. ; Blanken, Peter D. Less -
NOAA Program & Office:

NESDIS (National Environmental Satellite, Data, and Information Service) ; NCEI (National Centers for Environmental Information)

NESDIS (National Environmental Satellite, Data, and Information Service) ; NCEI (National Centers for Environmental Information) Less -
Description:

Precipitation changes the physiological characteristics of an ecosystem. Because land-surface models are often used to project changes in the hydrological cycle, modeling the effect of precipitation onthe latent heat ﬂux kEis an important aspect of land-surface models. Here we contrast conditionally sam- pled diel composites of the eddy-covariance ﬂuxes from the Niwot Ridge Subalpine Forest AmeriFlux tower with the Community Land Model (CLM, version 4.5). With respect to measured kEduring the warm season: for the day following above-average precipitation, kEwas enhanced at midday by /C2540 W m 22(relative to dry conditions), and nocturnal kEincreased from /C2510 W m22in dry conditions to over 20 W m22in wet
Keywords:

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Environmental Chemistry General Earth And Planetary Sciences Global And Planetary Change
Source:

Journal of Advances in Modeling Earth Systems, 10(3), 617-651
DOI:

https://doi.org/10.1002/2017MS001248
ISSN:

1942-2466;1942-2466;
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PDF
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American Geophysical Union (AGU)
Document Type:

Journal Article
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https://creativecommons.org/licenses/by-nc-nd/4.0/
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CC BY-NC-ND
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urn:sha256:43f4f7814243eb4a80841b575baa656be1ec1ebe10ee5d6550b14d6d26b5a93b
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https://repository.library.noaa.gov/view/noaa/52742/noaa_52742_DS1.pdf
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