Unprecedented acceleration of winter discharge of Upper Yenisei River inferred from tree rings

Irina P. Panyushkina, David M. Meko, Alexander Shiklomanov, Richard D. Thaxton, Vladimir Myglan, Valentin V. Barinov, Anna V. Taynik

Research output: Contribution to journalArticlepeer-review

Abstract

The Yenisei River is the largest contributor of freshwater and energy fluxes among all rivers draining to the Arctic Ocean. Modeling long-Term variability of Eurasian runoff to the Arctic Ocean is complicated by the considerable variability of river discharge in time and space, and the monitoring constraints imposed by a sparse gauged-flow network and paucity of satellite data. We quantify tree growth response to river discharge at the upper reaches of the Yenisei River in Tuva, South Siberia. Two regression models built from eight tree-ring width chronologies of Larix sibirica are applied to reconstruct winter (Nov-Apr) discharge for the period 1784-1997 (214 years), and annual (Oct-Sept) discharge for the period 1701-2000 (300 years). The Nov-Apr model explains 52% of the discharge variance whereas Oct-Sept explains 26% for the calibration intervals 1927-1997 and 1927-2000, respectively. This new hydrological archive doubles the length of the instrumental discharge record at the Kyzyl gauge and resets the temporal background of discharge variability back to 1784. The reconstruction finds a remarkable 80% upsurge in winter flow over the last 25 years, which is unprecedented in the last 214 years. In contrast, annual discharge fluctuated normally for this system, with only a 7% increase over the last 25 years. Water balance modeling with CRU data manifests a significant discrepancy between decadal variability of the gauged flow and climate data after 1960. We discuss the impact on the baseflow rate change of both the accelerating permafrost warming in the discontinuous zone of South Siberia and widespread forest fires. The winter discharge accounts for only one third of the annual flow, yet the persistent 25 year upsurge is alarming. This trend is likely caused by Arctic Amplification, which can be further magnified by increased winter flow delivering significantly more fresh water to the Kara Sea during the cold season.

Original languageEnglish (US)
Article number125014
JournalEnvironmental Research Letters
Volume16
Issue number12
DOIs
StatePublished - Dec 2021

Keywords

  • Arctic amplification
  • Siberian rivers
  • discharge tree-ring reconstruction
  • water balance model

ASJC Scopus subject areas

  • Renewable Energy, Sustainability and the Environment
  • Environmental Science(all)
  • Public Health, Environmental and Occupational Health

Fingerprint

Dive into the research topics of 'Unprecedented acceleration of winter discharge of Upper Yenisei River inferred from tree rings'. Together they form a unique fingerprint.

Cite this