The Karnali River is one of the major transboundary rivers of the Nepalese central Himalaya and a major tributary of the Ganges River. Though there is a huge potential for dendrohydrological research in the Karnali River Basin (KRB) region in Nepal. No multi-centuries streamflow reconstruction is available yet.
The study has been published in the Journal of Hydrology. Xishuangbanna Tropical Botanical Garden (XTBG) of the Chinese Academy of Sciences scientists presented the first multi-centennial spring- to early-summer season (March–July) streamflow reconstruction for the Karnali River in the central Himalaya by using moisture-sensitive tree ring-width chronologies of multiple tree species.
Scientists compiled eleven tree ring-width chronologies based on 354 exactly dated tree cores from five coniferous species for the Karnali River catchment.The tree-ring site chronologies from the Karnali River Basin showed high dendroclimatological potential.
The composite chronologies from the KRB were generally positively correlated with spring and early summer season precipitation and drought index and negatively correlated with spring season temperature. The growth of trees is mainly limited by the moisture availability during spring and early summer seasons.
The reconstruction revealed annual to multi-decadal fluctuations in the streamflow of the Karnali River. Several moderate and extreme flow years were also observed in their reconstruction. An increasing frequency of extreme events occurred during the recent decades.
Karnali river flow has short-term (inter-annual) to decadal periodicities. It is similar to frequencies of broad-scale climate modes/phases like El Niño-Southern Oscillation and the Pacific Decadal Oscillation.