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  1. Home

Coupling Remote Sensing With A Process Model For The Simulation Of Rangeland Carbon Dynamics

by Yushu Xia - April 17, 2025

Rangelands provide significant environmental benefits through many ecosystem services, which may include soil organic carbon (SOC) sequestration. However, quantifying SOC stocks and monitoring carbon (C) fluxes in rangelands are challenging… More

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Representativeness Of Eddy-Covariance Flux Footprints For Areas Surrounding Ameriflux Sites

by Housen Chu - March 18, 2021

Large datasets of greenhouse gas and energy surface-atmosphere fluxes measured with the eddy-covariance technique (e.g., FLUXNET2015, AmeriFlux BASE) are widely used to benchmark models and remote-sensing products. This study addresses… More

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Bengtsson, Carl

by Carl Bengtsson - July 17, 2020

in Year of Methane   NDIR 0

Recovering Evapotranspiration Trends From Biased CMIP5 Simulations And Sensitivity To Changing Climate Over North America

by Anonymous - July 31, 2019

Future projections of evapotranspiration (ET) are of critical importance for agricultural and freshwater management and for predicting land–atmosphere feedbacks on the climate system. However, ET from phase 5 of the… More

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Improved Spatiotemporal Representativeness And Bias Reduction Of Satellite-Based Evapotranspiration Retrievals Via Use Of In Situ Meteorology And Constrained Canopy Surface Resistance

by - March 29, 2019

Evapotranspiration (ET) is a key component of the atmospheric and terrestrial water and energy budgets. Satellite‐based vegetation index approaches have used remotely sensed vegetation and reanalysis meteorological properties with surface… More

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GUNTURU, Vamsi Krishna

by GUNTURU VAMSI KRISHNA - December 17, 2018

in Year of Methane   0

CO2 exchange and evapotranspiration across dryland ecosystems of southwestern North America

by Anonymous - April 18, 2017

Global-scale studies suggest that dryland ecosystems dominate an increasing trend in the magnitude and interannual variability of the land CO2 sink. However, such analyses are poorly constrained by measured CO2… More

in    0
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