Abstract

Abstract. We analyzed the seasonal variations of energy balance components over three different surfaces: irrigated cropland (Yingke, YK), alpine meadow (A'rou, AR), and spruce forest (Guantan, GT). The energy balance components were measured using eddy covariance (EC) systems and a large aperture scintillometer (LAS) in the Heihe River Basin, China, in 2008 and 2009. We also determined the source areas of the EC and LAS measurements with a footprint model for each site and discussed the differences between the sensible heat fluxes measured with EC and LAS at AR. The results show that the main EC source areas were within a radius of 250 m at all of the sites. The main source area for the LAS (with a path length of 2390 m) stretched along a path line approximately 2000 m long and 700 m wide. The surface characteristics in the source areas changed with the season at each site, and there were characteristic seasonal variations in the energy balance components at all of the sites. The sensible heat flux was the main term of the energy budget during the dormant season. During the growing season, however, the latent heat flux dominated the energy budget, and an obvious "oasis effect" was observed at YK. The sensible heat fluxes measured by LAS at AR were larger than those measured by EC at the same site. This difference seems to be caused by the so-called energy imbalance phenomenon, the heterogeneity of the underlying surfaces, and the difference between the source areas of the LAS and EC measurements.

Highlights

  • Energy and water vapor interactions between land surfaces and the atmosphere are the most crucial ecological processes in terrestrial ecosystems (Baldocchi et al, 1997)

  • The main contributing source area of the eddy covariance (EC) measurements for each month was within a 180 m radius of the observation point at YK, and the contribution ratio increased to a maximum approximately 30 m away from the observation point

  • At GT, the source areas of EC during each month extended from southwest to northeast, with the main contribution area localized within 460 m and 450 m

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Summary

Introduction

Energy and water vapor interactions between land surfaces and the atmosphere are the most crucial ecological processes in terrestrial ecosystems (Baldocchi et al, 1997). These interactions determine the long-range transport of heat, humidity, and pollutants, and the growth rate and properties of the planetary boundary layer (Wilson and Baldocchi, 2000). The eddy covariance (EC) method has been widely applied to measure the exchange of energy, water vapor, and carbon dioxide between the land surface and the atmosphere. This technique is considered a standard method for measuring surface fluxes (Aubinet et al, 2000). One of the most important problems is the “energy imbalance” in applying

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