- Main
Challenges and Future Directions in Quantifying Terrestrial Evapotranspiration
- Yi, Koong;
- Senay, Gabriel B;
- Fisher, Joshua B;
- Wang, Lixin;
- Suvočarev, Kosana;
- Chu, Housen;
- Moore, Georgianne W;
- Novick, Kimberly A;
- Barnes, Mallory L;
- Keenan, Trevor F;
- Mallick, Kanishka;
- Luo, Xiangzhong;
- Missik, Justine EC;
- Delwiche, Kyle B;
- Nelson, Jacob A;
- Good, Stephen P;
- Xiao, Xiangming;
- Kannenberg, Steven A;
- Ahmadi, Arman;
- Wang, Tianxin;
- Bohrer, Gil;
- Litvak, Marcy E;
- Reed, David E;
- Oishi, A Christopher;
- Torn, Margaret S;
- Baldocchi, Dennis
Published Web Location
https://doi.org/10.1029/2024wr037622Abstract
Abstract Terrestrial evapotranspiration is the second‐largest component of the land water cycle, linking the water, energy, and carbon cycles and influencing the productivity and health of ecosystems. The dynamics of ET across a spectrum of spatiotemporal scales and their controls remain an active focus of research across different science disciplines. Here, we provide an overview of the current state of ET science across in situ measurements, partitioning of ET, and remote sensing, and discuss how different approaches complement one another based on their advantages and shortcomings. We aim to facilitate collaboration among a cross‐disciplinary group of ET scientists to overcome the challenges identified in this paper and ultimately advance our integrated understanding of ET. Key Points The main challenge in ET science is reconciling spatial data with point data from various sources across heterogeneous areas Each of the three general approaches to ET science (in situ measurements, partitioning, remote sensing) has strengths and weaknesses Communication and translation across these disciplines are key to closing the gaps
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