The exchange of water, energy, and carbon between the land surface and the atmosphere is largely influenced by vegetation. In turn, vegetation is strongly influenced by the partitioning of precipitation into evapotranspiration, soil moisture, and runoff. Ultimately, the hydrologic cycle exerts a strong control on the climate system. In fact, positive feedbacks between vegetation and the hydrologic cycle at small scales may have the ability to elicit non-linear responses with important large scale consequences. Therefore, capturing the synergies between hydrologic processes at different space and time scales is necessary for appropriately modeling the influence of vegetation and the hydrologic cycle on the climate system. Understanding the controls on land-atmosphere interactions and how they influence larger scale feedbacks will become increasingly important as climatic and other global changes continue to alter the water availability of our ecosystems.
Water-limited ecosystems are especially sensitive to precipitation changes, and therefore insights concerning how their functioning responds to possible changes in precipitation patterns are important in understanding future climate scenarios. Over a decade of field work from my research group has highlighted the importance of deep soil moisture (from large storms) in the healthy functioning of water-limited ecosystems. This has led to the development of a two-layer soil moisture conceptual framework for exploring land surface-atmosphere interactions in water-limited ecosystems. Here I demonstrate how this framework can been used to link small scale processes investigated in field with large scale processes for water-limited ecosystems.
Papuga S. (2014): A two-layer soil moisture conceptual framework for exploring land surface-atmosphere interactions in water-limited ecosystem. Abstract H41H-07 presented at 2014 Fall Meeting, AGU, San Francisco, CA, 15-19 Dec..
This Paper/Book acknowledges NSF CZO grant support.