Passive microwave and optical index approaches for estimating surface conductance and evapotranspiration in forest ecosystems
In this study, we evaluated and compared optical and passive microwave index based retrievals of surface conductance (Gs) and evapotranspiration (ET) following the Penman-Monteith (PM) approach. The methodology was evaluated over the growing season at five FLUXNET sites in the USA and Australia enco...
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Elsevier B.V.
2015
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| LEADER | 17336caa a22012617a 4500 | ||
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| 001 | PAPER-24615 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250428091209.0 | ||
| 008 | 190411s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84936759508 | |
| 030 | |a AFMEE | ||
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Barraza, V. | |
| 245 | 1 | 0 | |a Passive microwave and optical index approaches for estimating surface conductance and evapotranspiration in forest ecosystems |
| 260 | |b Elsevier B.V. |c 2015 | ||
| 270 | 1 | 0 | |m Barraza, V.; Instituto de Astronomía y Física del Espacio (IAFE, CONICET-UBA), Pabellon IAFE, CABAArgentina; email: vbarraza@iafe.uba.ar |
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| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a In this study, we evaluated and compared optical and passive microwave index based retrievals of surface conductance (Gs) and evapotranspiration (ET) following the Penman-Monteith (PM) approach. The methodology was evaluated over the growing season at five FLUXNET sites in the USA and Australia encompassing three forest types, deciduous broadleaf forest (DBF), evergreen needleleaf forest (ENF) and evergreen broadleaf forest (EBF). A subset of Gs values were regressed against individual and combined indices of NDWI, EVI, and FI (microwave frequency index), and used to parameterize the PM equation for retrievals of ET (PM-Gs). For this purpose, we used MODIS (MYD09A1) and AMSR-E passive microwave data to compute the VIs. Model performance was quantitatively evaluated through comparative analysis of the regression coefficients (r2), and root mean square errors (RMSE). All indices correlated well with Gs over deciduous broadleaf forests, explaining 40-60% of Gs variations, however, the optical-based models had lower RMSE than the microwave FI model. In contrast, the FI model yielded the best performance to estimate Gs in evergreen forests (EBF and ENF). Overall, a combined microwave-optical model resulted in the best Gs estimates in these evergreen forests compared with the individual model approaches. In general, the PM-models explained more than 70% of the variance in LE with RMSE lower than 20W/m2. Based on these results, we developed a new approach combining optical and passive microwave indices based on their spatial vs. temporal synergies to generate Gs time series. This combined optical-microwave approach produced the best ET estimates for evergreen forest and offered a robust approach for deciduous forest without sacrificing precision. © 2015 Elsevier B.V. |l eng | |
| 536 | |a Detalles de la financiación: University of Sydney, ARC-DP140102698 | ||
| 536 | |a Detalles de la financiación: Part of this study was conducted through a visiting scholar appointment awarded to the author by the University of Technology, Sydney through funds from ARC-DP140102698 (Huete, CI) . This work was also funded by MinCyT-CONAE-CONICET project 12. The author thanks Fluxnet and Ozflux Network for making the data freely available as well as the flux tower principal investigators. Appendix A | ||
| 593 | |a Instituto de Astronomía y Física del Espacio (IAFE, CONICET-UBA), Pabellon IAFE, CABA, Buenos Aires, Argentina | ||
| 593 | |a Plant Functional Biology and Climate Change Cluster (C3), University of Technology Sydney (UTS), Broadway, NSW 2007, Australia | ||
| 593 | |a CSIRO Oceans and Atmosphere Flagship, Canberra, ACT, Australia | ||
| 651 | 4 | |a AUSTRALIA | |
| 690 | 1 | 0 | |a EVAPOTRANSPIRATION |
| 690 | 1 | 0 | |a MICROWAVE INDEX |
| 690 | 1 | 0 | |a OPTICAL INDICES |
| 690 | 1 | 0 | |a SURFACE CONDUCTANCE |
| 690 | 1 | 0 | |a AMSR-E |
| 690 | 1 | 0 | |a COMPARATIVE STUDY |
| 690 | 1 | 0 | |a ESTIMATION METHOD |
| 690 | 1 | 0 | |a EVAPOTRANSPIRATION |
| 690 | 1 | 0 | |a FOREST ECOSYSTEM |
| 690 | 1 | 0 | |a HYDRAULIC CONDUCTIVITY |
| 690 | 1 | 0 | |a INDEX METHOD |
| 690 | 1 | 0 | |a MICROWAVE RADIATION |
| 690 | 1 | 0 | |a MODEL TEST |
| 690 | 1 | 0 | |a MODIS |
| 690 | 1 | 0 | |a PARAMETERIZATION |
| 690 | 1 | 0 | |a PENMAN-MONTEITH EQUATION |
| 690 | 1 | 0 | |a PERFORMANCE ASSESSMENT |
| 690 | 1 | 0 | |a VEGETATION TYPE |
| 690 | 1 | 0 | |a UNITED STATES |
| 700 | 1 | |a Restrepo-Coupe, N. | |
| 700 | 1 | |a Huete, A. | |
| 700 | 1 | |a Grings, Francisco Matías | |
| 700 | 1 | |a Van Gorsel, E. | |
| 773 | 0 | |d Elsevier B.V., 2015 |g v. 213 |h pp. 126-137 |p Agric. For. Meterol. |x 01681923 |w (AR-BaUEN)CENRE-70 |t Agricultural and Forest Meteorology | |
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