A drought reconstruction from the low-elevation juniper forest of northwestern Kyrgyzstan since CE 1565

Abstract

Naryn River provides large amounts of water resource for Central Asian countries. Thus, the severity and frequency of drought variation relate to runoff has important influences on social and economic development of this region. In this study, the new tree-ring width chronologies of juniper trees from the low-elevation site of the western Tien Shan are used to reconstruct drought variation for northwestern Kyrgyzstan and place the short instrumental period (1950–2013) of Standardised Precipitation-Evapotranspiration Index (SPEI) in a long-term context. The SPEI reconstruction successfully reflects the dry and wet periods over the past 451 years, and captures a recent wetting trend that generally agrees with the drought reconstructions for the spruce-dominated area. However, some differences between the tree-ring records from spruce-dominated and juniper-dominated areas reflect regional climate differences. The comparison between drought events in the SPEI reconstruction and historical event of Central Asia reveals drought variations have had profound influences on some historical archives over the past several centuries. This study provides the first long-term SPEI reconstruction and drought evaluation from the low-altitude area of Central Asia, contributing to climate change issues in Central Asia.