Articles | Volume 13, issue 6
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-13-1635-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Jun 2019
Research article |
| 14 Jun 2019
| 14 Jun 2019
Warming temperatures are impacting the hydrometeorological regime of Russian rivers in the zone of continuous permafrost
Olga Makarieva
CORRESPONDING AUTHOR
Saint Petersburg State University, 7/9 Universitetskaya nab, St. Petersburg, 199034, Russia
Melnikov Permafrost Institute, Merzlotnaya St., 36, Yakutsk, 677010, Russia
Nataliia Nesterova
Saint Petersburg State University, 7/9 Universitetskaya nab, St. Petersburg, 199034, Russia
State Hydrological Institute, 23 2-ya liniya VO, St. Petersburg, 199053, Russia
David Andrew Post
Commonwealth Scientific and Industrial Research Organisation, GPO Box 1700, Canberra, Australia
Artem Sherstyukov
All-Russia Research Institute of Hydrometeorological Information – World Data Centre, 6 Korolyov St.,
Obninsk, Kaluga Region, 249035, Russia
Lyudmila Lebedeva
Melnikov Permafrost Institute, Merzlotnaya St., 36, Yakutsk, 677010, Russia
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43 citations as recorded by crossref.
- Changes in the wintertime hydroclimatic regime in St. John River, Maine, USA J. Kim et al. 10.2166/wcc.2021.230
- Heterogenous runoff trends in peatland-dominated basins throughout the circumpolar North M. Mack et al. 10.1088/2515-7620/ac11ed
- The impact of climate change on seasonal glaciation in the mountainous permafrost of North-Eastern Eurasia by the example of the giant Anmangynda aufeis A. Zemlianskova et al. 10.1016/j.catena.2023.107530
- Increasing Alaskan river discharge during the cold season is driven by recent warming D. Blaskey et al. 10.1088/1748-9326/acb661
- Permafrost Degradation and Its Hydrogeological Impacts H. Jin et al. 10.3390/w14030372
- A century of variations in extreme flow across Finnish rivers A. Gohari et al. 10.1088/1748-9326/aca554
- Mechanisms behind the uneven increases in early, mid- and late winter streamflow across four Arctic river basins S. Liu et al. 10.1016/j.jhydrol.2021.127425
- The Role of the Russian Shelf in Seasonal and Interannual Variability of Arctic Sea Surface Salinity and Freshwater Content S. Hall et al. 10.1029/2022JC019247
- The ice regime of the northeastern Russia A. Zemlianskova et al. 10.7256/2453-8922.2024.1.69791
- Permafrost dynamics and their hydrologic impacts over the Russian Arctic drainage basin K. Wang et al. 10.1016/j.accre.2021.03.014
- Parameterizing a hydrological model using a short‐term observational dataset to study runoff generation processes and reproduce recent trends in streamflow at a remote mountainous permafrost basin N. Nesterova et al. 10.1002/hyp.14278
- Eastern Siberia permafrost transect (ESPT). A first stage: The Verkhoyansk Range part R. Sysolyatin et al. 10.1007/s11629-023-7965-1
- Potential role of permafrost thaw on increasing Siberian river discharge P. Wang et al. 10.1088/1748-9326/abe326
- Streamflow Changes in the Headwater Area of Yellow River, NE Qinghai-Tibet Plateau during 1955–2040 and Their Implications Q. Ma et al. 10.3390/w13101360
- Influence of Large-scale Atmospheric Processes on Seasonal Runoff of Large Siberian Rivers L. Vasilevskaya et al. 10.3103/S1068373921100046
- Impacts of spatially inconsistent permafrost degradation on streamflow in the Lena River Basin Z. Xue et al. 10.1007/s11431-023-2757-2
- Brief communication: Alternation of thaw zones and deep permafrost in the cold climate conditions of the East Siberian Mountains, Suntar-Khayata Range R. Sysolyatin et al. 10.5194/tc-17-4601-2023
- Modeling of runoff formation processes with aufeis feed in mountain cryosphere of the north-east of Russia A. Zemlianskova & O. Makarieva 10.7256/2453-8922.2024.2.69780
- The distribution and dynamics of aufeis in permafrost regions T. Ensom et al. 10.1002/ppp.2051
- Frozen ground change and its potential influence on river discharge in the Tienshan Mountains, northwestern China X. Wang et al. 10.1080/02626667.2020.1851374
- Proglacial icings as records of winter hydrological processes A. Chesnokova et al. 10.5194/tc-14-4145-2020
- Geocryological Conditions of Small Mountain Catchment in the Upper Kolyma Highland (Northeastern Asia) O. Makarieva et al. 10.3390/geosciences14040088
- Seasonality of DOC Export From a Russian Subarctic Catchment Underlain by Discontinuous Permafrost, Highlighted by High‐Frequency Monitoring L. Gandois et al. 10.1029/2020JG006152
- Late Summer Water Sources in Rivers and Lakes of the Upper Yana River Basin, Northern Eurasia, Inferred from Hydrological Tracer Data N. Tananaev 10.3390/hydrology9020024
- Re-activation of landslide in sub-Arctic areas due to extreme rainfall and discharge events (the mouth of the Great Whale River, Nunavik, Canada) P. Owczarek et al. 10.1016/j.scitotenv.2020.140991
- Giant Aufeis—Unknown Glaciation in North-Eastern Eurasia According to Landsat Images 2013–2019 O. Makarieva et al. 10.3390/rs14174248
- The effect of climate change on sources of radionuclides to the marine environment J. Gwynn et al. 10.1038/s43247-024-01241-w
- Shallow and deep groundwater moderate methane dynamics in a high Arctic glacial catchment G. Kleber et al. 10.3389/feart.2024.1340399
- Evidence of Hydrological Intensification and Regime Change From Northern Alaskan Watershed Runoff C. Arp et al. 10.1029/2020GL089186
- Changes in permafrost and snow cover in the Boreal and Arctic zones (BAZs) and their impacts H. Jin et al. 10.1016/j.accre.2023.04.002
- Modeling of the Summer 2019 Disastrous Floods on the Iya River (Irkutsk Oblast) O. Makarieva et al. 10.1134/S187537284104006X
- The Fate of Stationary Tools for Environmental Flow Determination in a Context of Climate Change A. St-Hilaire et al. 10.3390/w13091203
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- Recent streamflow trends across permafrost basins of North America K. Bennett et al. 10.3389/frwa.2023.1099660
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Latest update: 14 Nov 2024
Short summary
The streamflow of Arctic rivers is changing. We analyzed available data (22 gauges, 1936–2015) in the basins of the Yana and Indigirka rivers completely located within the continuous permafrost zone. The results show that the main factor of increasing low flows is the shift from snow to rain due to warming. Other factors related to the release of water from permafrost, glaciers, or aufeis may fractionally contribute to streamflow increase but cannot be quantified based on available data.
The streamflow of Arctic rivers is changing. We analyzed available data (22 gauges, 1936–2015)...
