Abstract

The Kunduz River is one of the main tributaries of the Amu Darya Basin in North Afghanistan. Many communities live in the Kunduz River Basin (KRB), and its water resources have been the basis of their livelihoods for many generations. This study investigates climate change impacts on the KRB catchment. Rare station data are, for the first time, used to analyze systematic trends in temperature, precipitation, and river discharge over the past few decades, while using Mann–Kendall and Theil–Sen trend statistics. The trends show that the hydrology of the basin changed significantly over the last decades. A comparison of landcover data of the river basin from 1992 and 2019 shows significant changes that have additional impact on the basin hydrology, which are used to interpret the trend analysis. There is considerable uncertainty due to the data scarcity and gaps in the data, but all results indicate a strong tendency towards drier conditions. An extreme warming trend, partly above 2 °C since the 1960s in combination with a dramatic precipitation decrease by more than −30% lead to a strong decrease in river discharge. The increasing glacier melt compensates the decreases and leads to an increase in runoff only in the highland parts of the upper catchment. The reduction of water availability and the additional stress on the land leads to a strong increase of barren land and a reduction of vegetation cover. The detected trends and changes in the basin hydrology demand an active management of the already scarce water resources in order to sustain water supply for agriculture and ecosystems in the KRB.

Highlights

  • Afghanistan is a semi-arid country with high variability and irregularity in precipitation

  • Little literature is available on climate change impacts in Afghanistan; some recently conducted

  • The study results indicate that, since the 1960s, the annual average temperature in the Kunduz River Basin (KRB) has been increasing, while precipitation and river discharge have been decreasing, with the exception of glacier-fed headwaters

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Summary

Introduction

Afghanistan is a semi-arid country with high variability and irregularity in precipitation. The Kunduz river is one of the main tributaries of the Amu Darya in North Afghanistan It is mainly nourished by snow and glaciers melting during spring and summer (Figure 1). In the year 2019, early rainfall in upper parts of the catchments, combined with increased snowmelt due to high temperatures, caused strong flooding in most river basins of the Amu. Darya tributaries in Afghanistan, with approximately 124,500 people affected and many killed [5]. Little literature is available on climate change impacts in Afghanistan; some recently conducted studies indicate a distinct warming trend and a decrease of rainfall in some parts of the country [6,7]. Studies indicate a distinct warming trend and a decrease of rainfall in some parts of the country [6, The first detailed and systematic analysis of climate data for Afghanistan that was conducted by.

Afghanistan
Kunduz River Basin
Climate
Hydrology
Data and Methods
Land Cover Classification
Change in Temperature and Precipitation
Changes
Changes in Discharge
Change
Constraints Due to Limited Data Availability
Climate Change Impacts
Conclusions and Recommendations

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