3 - Soil–vegetation–atmosphere parameterizations

Summary

Introduction

Evolution teaches us that organisms must come to terms with their environment in order to grow and reproduce successfully. This suggests that many, if not all, successful organisms have strategies that allow them to adapt to changing environmental conditions. Unfortunately, when an organism interacts with its environment, the physical processes are rarely simple and the physiological mechanisms often are poorly understood. This is the challenge one faces when trying to incorporate vegetation into numerical models.

The atmosphere and vegetation interact in a number of different ways, and many of these need to be parameterized. The main five ways in which they interact are via the biophysical control of evapotranspiration, momentum transfer, soil moisture availability, radiation, and insulation (Sellers et al. 1986). The discussion of soil–vegetation–atmosphere parameterizations is organized around these five interaction types.

Biophysical control of evapotranspiration

Plants use photosynthetically active radiation, part of shortwave radiative energy, to combine water and carbon dioxide (CO₂) into sugars and other organic compounds. Thus, plants must allow for the transfer of CO₂ from the atmosphere to the cellular sites of photosynthesis. By doing so, plants expose their saturated tissues to the atmosphere and water loss occurs. Plants regulate the amount of CO₂ exchanged, and therefore regulate water loss, by means of valve-like structures on the leaf surface called stomates. Some plants have stomates on both sides of the leaf; others on only one side.