Novick Kimberly A, Ficklin Darren L, Baldocchi Dennis, Davis Kenneth J, Ghezzehei Teamrat A, Konings Alexandra G, MacBean Natasha, Raoult Nina, Scott Russell L, Shi Yuning, Sulman Benjamin N, Wood Jeffrey D
O'Neill School of Public and Environmental Affairs, Indiana University - Bloomington. Bloomington, IN USA.
Department of Geography, Indiana University - Bloomington. Bloomington, IN USA.
Nat Geosci. 2022 Mar;15(3):158-164. doi: 10.1038/s41561-022-00909-2. Epub 2022 Mar 11.
Water potential directly controls the function of leaves, roots, and microbes, and gradients in water potential drive water flows throughout the soil-plant-atmosphere continuum. Notwithstanding its clear relevance for many ecosystem processes, soil water potential is rarely measured in-situ, and plant water potential observations are generally discrete, sparse, and not yet aggregated into accessible databases. These gaps limit our conceptual understanding of biophysical responses to moisture stress and inject large uncertainty into hydrologic and land surface models. Here, we outline the conceptual and predictive gains that could be made with more continuous and discoverable observations of water potential in soils and plants. We discuss improvements to sensor technologies that facilitate in situ characterization of water potential, as well as strategies for building new networks that aggregate water potential data across sites. We end by highlighting novel opportunities for linking more representative site-level observations of water potential to remotely-sensed proxies. Together, these considerations offer a roadmap for clearer links between ecohydrological processes and the water potential gradients that have the 'potential' to substantially reduce conceptual and modeling uncertainties.
水势直接控制着叶片、根系和微生物的功能,水势梯度驱动着水分在整个土壤-植物-大气连续体中的流动。尽管土壤水势与许多生态系统过程密切相关,但很少进行原位测量,而植物水势观测通常是离散、稀疏的,尚未汇总到可访问的数据库中。这些差距限制了我们对生物物理对水分胁迫响应的概念理解,并给水文和陆面模型带来了很大的不确定性。在这里,我们概述了通过对土壤和植物水势进行更连续和可发现的观测所能取得的概念性和预测性进展。我们讨论了有助于原位表征水势的传感器技术的改进,以及建立跨站点汇总水势数据的新网络的策略。最后,我们强调了将更具代表性的站点级水势观测与遥感代理联系起来的新机会。这些考虑共同为生态水文过程与水势梯度之间建立更清晰联系提供了路线图,而水势梯度“有可能”大幅减少概念和建模的不确定性。