Strength and Sensitivity of Land-Atmosphere Interaction

TL;DR

This paper explores the theoretical and empirical relationships between land-atmosphere coupling strength and sensitivity, emphasizing the importance of coupling sensitivity in understanding climate variability and extreme events.

Contribution

It distinguishes coupling strength from sensitivity, providing a theoretical framework and empirical evidence highlighting the significance of coupling sensitivity in climate dynamics.

Findings

Soil moisture variances are highest in transitional climate zones.

Coupling sensitivity can be high even in non-hotspot regions.

Understanding coupling sensitivity is crucial for predicting extreme climate events.

Abstract

The land-atmosphere coupling strength has been defined as the percentage of precipitation variability explained by the variation of soil moisture in the Global Land-Atmosphere Coupling Experiment (GLACE). While it is useful to identify global hotspots of land-atmosphere interaction, this coupling strength is different from coupling sensitivity, which directly quantifies how precipitation generation responds to the perturbation of soil moisture and is essential for our understanding of the global water cycle. To disentangle these two quantities, here we theoretically explore the relationships among coupling strength, sensitivity, and soil moisture variances. We use climate model outputs to show that the largest soil moisture variances are located in the transitional climate zones and the variations of soil moisture largely account for the geographical patterns of coupling hotspots. The coupling sensitivity is not necessarily low in non-hotspot regions, which could impose great impacts on the development of extreme climate events. We therefore call for more research attention on coupling sensitivity to improve our understanding of the climate system.