Abstract

Investigating the energy and water vapor exchange in oasis riparian forest ecosystems is of significant importance to improve scientific understanding of land surface processes in extreme arid regions. The Heihe Watershed Allied Telemetry Experimental Research (HiWATER) provided many observations of water vapor and heat fluxes from riparian forest ecosystem by using a network of eddy-covariance (EC) systems installed over representative surfaces in the Ejina Oasis, which is located in the downstream areas of the Heihe River Basin, northwestern China. Based on EC flux measurements and meteorological data performed at five stations and covering representative surface types of Populus euphratica tree with associated Tamarix chinensis shrub, Tamarix chinensis shrubland, cantaloupe cropland, and barren-land, this study explored the spatio-temporal patterns of heat and water vapor fluxes over the Ejina Oasis riparian forest ecosystem with five different surface types over the course of a growing season in 2014. Energy balance closure of the flux data was evaluated; footprint analysis for each EC site was also performed. Results showed that energy balance closure for the flux data was reasonably good, with average energy balance ratio (EBR) of 1.03. The seasonal variations in net radiation (Rn), latent (LE), and sensible heat flux (H) over the five contrasting surfaces were similar, and a reverse seasonal change was observed in energy partitioning into LE and H. Remarkable differences in Rn, LE, and H between the five surfaces were explored preliminarily, associated closely with the soil properties and foliage phenology. Over the growing season (May–October) in 2014, the total ET ranged 622–731 mm for mixed forest of P. euphratica trees with associated T. chinensis shrubs with average daily ET of 3.6–4.2 mm; ET from T. chinensis shrubland was about 541 mm, with average daily ET of 3.6 mm. ET for barren-land was 195 mm. The total ET in irrigated cantaloupe cropland with plastic mulch was 431 mm for its four-month growing period with a total average of 3.8 mm d−1. Determination of ET over riparian forest ecosystem helps to improve reasonable use of limited water resource in the Ejina Oasis.

Highlights

  • The terrestrial ecosystem latent and sensible heat fluxes strongly interact with the overlaying atmosphere and affect the characteristics of the planetary boundary layer [6], influencing the local and even regional climate [1,3,7,8]

  • BasedBased on continuous measurements of meteorological ical measurements and turbulent on continuous measurements of meteorofactors, water vapor and energy flux, and groundwater depth, this study focused on logical factors, water vapor and energy flux, and groundwater depth, this study focused investigating the temporal patterns of energy fluxes exchanges and evapotranspiration on investigating the temporal patterns of energy fluxes exchanges and evapotranspiration over overthe theEjina

  • For barren-land, more than 40% of net radiation was partitioned into sensible heat flux for the whole growing season

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Summary

Introduction

Many important processes of terrestrial ecosystems, such as photosynthesis and evapotranspiration, are associated with the energy and mass exchange between the land surface and atmosphere [1,2,3,4]. The terrestrial ecosystem latent and sensible heat fluxes strongly interact with the overlaying atmosphere and affect the characteristics of the planetary boundary layer [6], influencing the local and even regional climate [1,3,7,8]. The water vapor and energy fluxes can be altered by local environmental variables that affecting a variety of physical and physiological processes in plants [3,4,5,7]. Land evapotranspiration (ET)/latent heat flux (in form of energy) is an essential component of the energy and water budgets in terrestrial ecosystems. Accurate quantification of ET is of great importance to water resources management, in areas of water scarcity [11,12]

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