Abstract

Abstract. Changes in land use and land cover (LULC) have been occurring at an accelerated pace in northern parts of China. These changes are significantly impacting the hydrology of these parts, such as Laohahe Catchment. The hydrological effects of these changes occurring in this catchment were investigated using a semi-distributed hydrological model. The semi-distributed hydrological model was coupled with a two-source potential evaportranspiration (PET) model for simulating daily runoff. Model parameters were calibrated using hydrometeorological and LULC data for the same period. The LULC data were available for 1980, 1989, 1996 and 1999. Daily streamflow measurements were available from 1964 to 2005 and were divided into 4 periods: 1964–1979, 1980–1989, 1990–1999 and 2000–2005. These periods represented four different LULC scenarios. Streamflow simulation was conducted for each period under these four LULC scenarios. The results showed that the change in LULC influenced evapotranspiration (ET) and runoff. The LULC data showed that from 1980 to 1996 grass land and water body had decreased and forest land and crop land had increased. This change caused the evaporation from vegetation interception and vegetation transpiration to increase, whereas the soil evaporation tended to decrease. Thus during the period of 1964–1979 the green water or ET increased by 0.95%, but the blue water or runoff decreased by 8.71% in the Laohahe Catchment.

Highlights

  • Blue water is the visible liquid water moving above the ground as surface runoff and below the ground as groundwater runoff (FAO, 1995b; Falkenmark and Rockstrom, 2004)

  • Green water is defined as the invisible vapor moving to the atmosphere (FAO, 1995a; Falkenmark and Rockstrom, 2004), including productive green water defined as transpiration from plants and trees, and nonproductive green water consisting of soil evaporation and vegetation interception evaporation

  • The objective of this study was to investigate the effect of land use and land cover (LULC) changes on the hydrological processes in the Laohahe Catchment in northern China by using a semi-distributed hydrological model coupled with a two-source potential evaportranspiration (PET) model

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Summary

Introduction

Blue water is the visible liquid water moving above the ground as surface runoff and below the ground as groundwater runoff (FAO, 1995b; Falkenmark and Rockstrom, 2004). Green water is defined as the invisible vapor moving to the atmosphere (FAO, 1995a; Falkenmark and Rockstrom, 2004), including productive green water defined as transpiration from plants and trees, and nonproductive green water consisting of soil evaporation and vegetation interception evaporation. It is a new concept to partition water into blue water and green water, which may effectively be utilized to study the effect of LULC changes on the catchment water balance. Quantification of the effect of LULC changes on the partition of blue water and green water of a river basin has been of interest to hydrologists in recent years. The conversion of rainfall into runoff is complex and our understanding of the quantitative relationship between the LULC properties and runoff generation mechanism is far from complete

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