Abstract

Precisely quantitative assessments of stream flow response to climatic change and permafrost thawing are highly challenging and urgent in cold regions. However, due to the notably harsh environmental conditions, there is little field monitoring data of runoff in permafrost regions, which has limited the development of physically based models in these regions. To identify the impacts of climate change in the runoff process in the Three-River Headwater Region (TRHR) on the Qinghai-Tibet Plateau, two artificial neural network (ANN) models, one with three input variables (previous runoff, air temperature, and precipitation) and another with two input variables (air temperature and precipitation only), were developed to simulate and predict the runoff variation in the TRHR. The results show that the three-input variable ANN model has a superior real-time prediction capability and performs well in the simulation and forecasting of the runoff variation in the TRHR. Under the different scenarios conditions, the forecasting results of ANN model indicated that climate change has a great effect on the runoff processes in the TRHR. The results of this study are of practical significance for water resources management and the evaluation of the impacts of climatic change on the hydrological regime in long-term considerations.

Highlights

  • Worldwide hydrological processes have been significantly affected by climate change

  • By using the monthly average temperature, monthly average precipitation, and previous monthly average runoff as driving factors, the performances of the artificial neural network (ANN) models for forecasting the 1, 3, 6, 12- and 24-month-ahead runoff variations for the Yellow River Headwater Region (YERHR), Yangtze River Headwater Region (YARHR), and Lantsang River Headwater Region (LARHR) are summarized in Tables 4, 5, and 6, respectively

  • For prediction of the runoff in the Three-River Headwater Region (TRHR), two ANN models were developed in this study

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Summary

Introduction

Worldwide hydrological processes have been significantly affected by climate change. There is significant complexity in physical interactions between thermal, hydrological, and hydrogeological effects in permafrost-affected regions [2]. The main feature of the long-term fluctuations in discharge of most Arctic rivers is an increase [5]. The long-term variation trend in runoff in the permafrost areas of the Qinghai-Tibet Plateau is a decrease [8]. Because of the minor human intervention (e.g., reservoirs, dams, and agricultural irrigation), the main reason for these tendencies is regional changes in climate conditions during the last 30 years [5, 9]. Little is known about the differences in the effects of climate changes on surface runoff in different permafrost regions [4, 7]

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