Spatiotemporal variability of palmer drought severity index inferred from long tree-ring chronologies in the Russian and Mongolian parts of the lake Baikal basin
https://doi.org/10.24057/2071-9388-2026-4381
Abstract
The spatiotemporal variability of moisture conditions in the Lake Baikal basin, a key region of Inner Asia, remains insufficiently understood due to the short duration of instrumental observations and the complex interplay of climatic factors. In this study, we reconstructed the self-calibrating Palmer Drought Severity Index (PDSI) for May–July using four long tree-ring chronologies from the Russian and Mongolian parts of the Baikal basin. Linear models explain 34–57% of the interannual variance in the instrumental PDSI. The 11-year smoothed mean PDSI values reveal alternating periods of in-phase and out-of-phase moisture variability between the two parts of the basin over the past ~250 years, while long-term (30-year) series show divergent trends: increasing moisture availability in the northern (BRG) and southwestern (HEC) parts of the basin and intensifying aridization in the central-southern part (KST, KRN). Several extreme drought (1863, 1923, and 2003) and wet (1938) years with broad spatial extent were identified. Spectral analysis of the reconstructed series revealed significant cycles of approximately 2–5 years and 14–56 years. The results of this study demonstrate substantial spatial heterogeneity in drought dynamics and highlight the influence of both local and large‑scale climatic factors on moisture regimes in Baikal Asia.
About the Authors
S. A. SatRussian Federation
6 Sakhyanovoi St., Ulan-Ude, 670047
A. A. Ayurzhanaev
Russian Federation
6 Sakhyanovoi St., Ulan-Ude, 670047
S. G. Andreev
Russian Federation
6 Sakhyanovoi St., Ulan-Ude, 670047
B. V. Sodnomov
Russian Federation
6 Sakhyanovoi St., Ulan-Ude, 670047
References
1. Alymbaeva Zh. B., Andreeva A.M., Ayurzhanaev A.A., Ayusheeva S.N., Bardakhanova T.B., et al. (Eds.) (2024). Impact of the Changing Water Level of Lake Baikal on the Economy and Ecosystems. Novosibirsk: Siberian Branch of the Russian Academy of Sciences, Baikal Institute of Nature Management, SB RAS. ISBN 978-5-6050995-5-0. DOI:10.53954/9785605099550.
2. Andreev S.G., Vaganov E.A., Naurzbaev M.M., and Tulokhonov A.K. (1999). Registration of long-term variations in atmospheric precipitation, Selenga River runoff, and Lake Baikal level by annual pine tree rings. Doklady Earth Sciences, 368(5), 1008–1011. (Transl. from Doklady RAN, 369(6), 825–828).
3. Andreev S.G., Vaganov E.A., Naurzbaev M.M., and Tulokhonov A.K. (2001). Radial growth of trees as an indicator of long-term changes in the hydrological regime in the Lake Baikal basin. Geography and Natural Resources, (4), 49–54. (In Russian).
4. Andreev S.G., Ayurzhanaev A.A., Batotsyrenov E.A., et al. (2022). Dendrochronological study of a 19th-century staging barn (Ethnographic Museum of the Peoples of Transbaikalia, Ulan-Ude). Journal of Siberian Federal University. Biology, 15(2), 279–292. https://doi.org/10.17516/1997-1389-0387 (In Russian).
5. Antokhina O.Y., Antokhin P.N., Martynova Y.V., and Mordvinov V.I. (2019). The linkage of precipitation in the Selenga River Basin to midsummer atmospheric blocking. Atmosphere, 10(6), 343. https://doi.org/10.3390/atmos10060343
6. Antokhina O., Antokhin P., Gochakov A., Zbirannik A., and Gazimov T. (2023). Atmospheric circulation patterns associated with extreme precipitation events in Eastern Siberia and Mongolia. Atmosphere, 14(3), 480. https://doi.org/10.3390/atmos14030480
7. Belokopytova L., Zhirnova D., Kostyakova T., and Babushkina E. (2018). Dynamics of moisture regime and its reconstruction from a treering width chronology of Pinus sylvestris in the downstream Selenga basin, Russia. Journal of Arid Land, 10, 877–891. https://doi.org/10.1007/s40333-018-0025-y
8. Cook E.R. and Kairiukstis L.A. (1990). Methods of Dendrochronology. Applications in the Environmental Sciences. International Institute for Applied Systems Analysis. Kluwer Academic Publishers, Dordrecht, 394 p. http://dx.doi.org/10.1007/978-94-015-7879-0
9. Cook E.R., Anchukaitis K.J., Buckley B.M., D’Arrigo R.D., Jacoby G.C., Wright W.E. (2010). Asian monsoon failure and megadrought during the last millennium. Science 328, 486–489. https://doi.org/10.1126/science.1185188
10. Chalov S.R., Jarsjö J., Kasimov N.S., et al. (2015). Spatio-temporal variation of sediment transport in the Selenga River Basin, Mongolia and Russia. Environmental Earth Sciences, 73, 663–680. https://doi.org/10.1007/s12665-014-3106-z
11. Chalov S., Thorslund J., Kasimov N.S., et al. (2016). The Selenga River delta: A geochemical barrier protecting Lake Baikal waters. Regional Environmental Change, 17(7), 2039–2053. https://doi.org/10.1007/s10113-016-0996-1
12. Dai A. (2021). Hydroclimatic trends during 1950–2018 over global land. Climate Dynamics, 56, 4027–4049. https://doi.org/10.1007/s00382-021-05684-1
13. Davi N.K., Jacoby G.C., Curtis A.E., and Baatarbileg N. (2006). Extension of drought records for Central Asia using tree rings: West-central Mongolia. Journal of Climate, 19(2), 288–299. https://doi.org/10.1175/JCLI3621.1
14. Davi N.K., Jacoby G.C., Fang K., et al. (2010). Reconstructing drought variability for Mongolia based on a large-scale tree-ring network: 1520–1993. Journal of Geophysical Research: Atmospheres, 115(D22), D22103. https://doi.org/10.1029/2010JD013907
15. Davi N.K., Pederson N., Leland C., Nachin B., Suran B., and Jacoby G.C. (2013). Is eastern Mongolia drying? A long-term perspective of a multidecadal trend. Water Resources Research, 49(1), 151–158. https://doi.org/10.1029/2012WR011834
16. Demina A.V., Belokopytova L.V., Andreev S.G., et al. (2017). Radial increment dynamics of Scots pine (Pinus sylvestris L.) as an indicator of hydrothermal regime of the Western Transbaikalia forest steppe. Contemp. Probl. Ecol. 10, 476–487. https://doi.org/10.1134/S1995425517050031
17. Demina A.V., Belokopytova L.V., Zhirnova D.F., Mehrotra N., Shah S.K., Babushkina E.A. and Vaganov E.A. (2022). Degree of connectivity in reconstructed precipitation dynamics and extremes for semiarid regions across South Siberia. Dendrochronologia, 71, 125903. https://doi.org/10.1016/j.dendro.2021.125903
18. Dolgova E.A., Solomina O.N., Matskovsky V.V., Dobryansky A.S., Semenyak N.A., and Shpunt S.S. (2019). Spatial variation of pine treering growth in the Solovetsky Islands. Izvestiya RAN. Seriya Geograficheskaya, 2, 41–50. https://doi.org/10.31857/S2587-55662019241-50 (In Russian, with English summary).
19. Ecological Atlas of Lake Baikal. (2015). Irkutsk: SB RAS Press, 145 p. (In Russian).
20. Edelgeriev R.S.-Kh., Ivanov A.L., Donnik I.M., et al. (2021). Global climate and the soil cover of Russia: Manifestations of drought, prevention, mitigation, elimination of consequences, and adaptation measures (agriculture and forestry). Moscow: MBA Publishing, 700 pp. (In Russian).
21. Fang K., Cook E., Guo Z., Chen D., Ou T., and Zhao Y. (2018). Synchronous multi-decadal climate variability of the whole Pacific areas revealed in tree rings since 1567. Environmental Research Letters, 13, 024016. DOI 10.1088/1748-9326/aa9f74
22. Fritts H.C. (1976). Tree Rings and Climate. London: Academic Press, 567 pp.
23. Frolova N.L., Belyakova P.A., Grigor’ev V.Y., Sazonov A.A., Zotov L.V., and Jarsjö J. (2017). Many-year variations of river runoff in the Selenga basin. Water Resources, 44, 359–371. https://doi.org/10.1134/S0097807817030101
24. Frolova N.L., Belyakova P.A., Grigoriev V.Yu., Sazonov A.A., Zotov L.V., and Jarsjö J. (2017b). Runoff fluctuations in the Selenga River Basin. Regional Environmental Change, 17, 1965–1976. https://doi.org/10.1007/s10113-017-1199-0
25. Garmaev E.Zh. (2010). Drainage of the Rivers of the Lake Baikal. - Ulan-Ude: Buryat State University Publishing Department, 272 p. (In Russian).
26. Gazol A., Camarero J.J., Sangüesa-Barreda G., Serra-Maluquer X., Sánchez-Salguero R., Coll L., and Casals P. (2020). Tree species are differently impacted by cumulative drought stress and present higher growth synchrony in dry places. Frontiers in Forests and Global Change, 3:573346. doi: 10.3389/ffgc.2020.573346
27. Gelfan A., Frolova M., Magritsky D., Kireeva M., Grigoriev V., Motovilov Yu., and Gusev E. (2021). Climate change impact on annual and maximum runoff of Russian rivers: diagnosis and projections. Fundamental and Applied Climatology, 7(1), 36–79. (In Russian).
28. Haraguchi M., Davi N., Rao M. P., Leland C., Watanabe M., and Lall U. (2022). Estimating return intervals for extreme climate conditions related to winter disasters and livestock mortality in Mongolia. Natural Hazards and Earth System Sciences, 22(8), 2751–2770. https://doi.org/10.5194/nhess-22-2751-2022
29. Harris I., Osborn T.J., Jones P. et al. (2020). Version 4 of the CRU TS monthly high-resolution gridded multivariate climate dataset. Sci Data 7(1), 109. https://doi.org/10.1038/s41597-020-0453-3
30. Hessl A.E., Anchukaitis K.J., Jelsema C., et al. (2018). Past and future drought in Mongolia. Science Advances, 4(3), e1701832. https://doi.org/10.1126/sciadv.1701832
31. Kasimov N.S., Shinkareva G., Lychagin M., Chalov S., Pashkina M., Thorslund J., and Jarsjö J. (2020). River water quality of the Selenga–Baikal Basin. Part II—Metal partitioning under different hydroclimatic conditions. Water, 12(9), 2392. https://doi.org/10.3390/w12092392
32. Kuznetsova V.V., Pozhidaeva D.S. (2017). Possibilities and limitations of reconstruction of river flow and aridity conditions in the Volga region by dendrochronological methods. Fundamental and Applied Climatology, 4, 46-65. DOI: 10.21513/2410-8758-2017-4-46-65 (In Russian).
33. Leland C., Pederson N., Nachin B., Hessl A., Saladyga T., and Suran B. (2013). A hydroclimatic regionalization of central Mongolia as inferred from tree rings. Dendrochronologia, 31(3), 205–215. https://doi.org/10.1016/j.dendro.2012.11.003
34. Li W., Jiang Y., Lin Z., Wang J., Zhang Y., and Ma W. (2024). Warming-driven increased synchrony of tree growth across the southernmost part of the Asian boreal forests. Science of the Total Environment, 938, 173389. https://doi.org/10.1016/j.scitotenv.2024.173389
35. Liu Y., Song H., Lei Y., et al. (2019). The 600-mm precipitation isoline distinguishes tree-ring-width responses to climate in China. National Science Review, 6(2), 359–368. https://doi.org/10.1093/nsr/nwy101
36. Mizandrontseva K.N. (1985). Climate of Lake Baikal in weather patterns. Novosibirsk: Nauka, 160 pp. (In Russian).
37. Muffler L., Weigel R., Hacket-Pain A.J., Klisz M., van der Maaten E., Wilmking M., Kreyling J., and van der Maaten-Theunissen M. (2020). Lowest drought sensitivity and decreasing growth synchrony towards the dry distribution margin of European beech. Journal of Biogeography, 47(9), 1910–1921. DOI:10.1111/jbi.13884
38. Narangerel S., Suzuki Y., Taniguchi K., et al. (2025). Floods and related problems after the 1980s in Khovd, Western Mongolia. Nat. Hazards, 121, 23627–23646. https://doi.org/10.1007/s11069-024-07033-x
39. Palmer W.C. (1965). Meteorological drought, Res. Pap., 45, U.S. Dept. of Commer. Weather Bur., Washington, D. C.
40. Pederson N., Jacoby G.C., D’Arrigo R.D., Cook E.R., Buckley B.M., Dugarjav C., and Mijiddorj R. (2001). Hydrometeorological reconstructions for northeastern Mongolia derived from tree rings: AD 1651–1995. Journal of Climate, 14(5), 978-991. https://doi.org/10.1175/1520-0442(2001)014<0872:HRFNMD>2.0.CO;2
41. Pederson N., Hessl A.E., Baatarbileg N., Anchukaitis K.J., and Di Cosmo, N. (2014). Pluvials, droughts, the Mongol Empire, and modern Mongolia. Proceedings of the National Academy of Sciences of the United States of America, 111(12), 4375-4379. https://doi.org/10.1073/pnas.1318677111
42. Roshydromet. (2014). Second Roshydromet Assessment Report on Climate Change and Its Consequences for the Russian Federation. Moscow: Roshydromet, 1004 pp. (In Russian).
43. Sangüesa-Barreda G., Camarero J.J., Sánchez-Salguero R. et al. (2019). Droughts and climate warming desynchronize Black pine growth across the Mediterranean Basin. Science of the Total Environment, 697. 133989. DOI: 10.1016/j.scitotenv.2019.133989
44. Sardans J., Miralles A., Tariq A., et al. (2024). Growing aridity poses threats to global land surface. Communications Earth & Environment, 5, 776. https://doi.org/10.1038/s43247-024-01935-1
45. Serdyanjiv N., Suzuki Y., Higurashi T., and Tanaka Y. (2024). Flood hazard mapping and disaster-prevention recommendations based on detailed topographical analysis in Khovd City, Western Mongolia. Natural Hazards and Earth System Sciences Discussions (preprint). https://doi.org/10.5194/nhess-2024-91
46. Shestakova T.A., Gutiérrez E., Kirdyanov A.V., Camarero J.J., Génova M., Knorre A.A., Linares J.C., Resco de Dios V., Sánchez-Salguero R., and Voltas J. (2016). Forests synchronize their growth in contrasting Eurasian regions in response to climate warming, Proc. Natl. Acad. Sci., 113 (3), 662-667. https://doi.org/10.1073/pnas.1514717113
47. Shestakova T.A., Gutiérrez E., Valeriano C., Lapshina E., and Voltas J. (2019). Recent loss of sensitivity to summer temperature constrains tree growth synchrony among boreal Eurasian forests. Agricultural and Forest Meteorology, 268, 318–330. https://doi.org/10.1016/j.agrformet.2019.01.039
48. Shigimaga, A.A., Bykov, N.I. and Rygalova, N.V. (2024). Features of Radial Growth of Trees in Shelterbelts of the Dry Steppe. Arid Ecosyst., 14, 463–472. https://doi.org/10.1134/S2079096124700434
49. Tabakova M., Arzac A., Martínez E., and Kirdyanov A. (2020). Climatic factors controlling Pinus sylvestris radial growth along a transect of increasing continentality in southern Siberia. Dendrochronologia, 62, 125709. https://doi.org/10.1016/j.dendro.2020.125709
50. Tejedor E., Serrano-Notivoli R., de Luis M., et al. (2020). A global perspective on the climate-driven growth synchrony of neighboring trees. Global Ecology and Biogeography, 29(7), 1114-1125. DOI:10.1111/geb.13090
51. Tsydypov B.Z., Garmaev E.Zh., Gomboev B.O., et al. (2022). Impact of climate change on ecosystem services of forest lands in the south of Eastern Siberia. Izvestiya RAN. Seriya Geograficheskaya, 86(1), 82–97. https://doi.org/10.31857/S2587556622010125 (In Russian).
52. Vaganov E.A., Shiyatov S.G., Mazepa V.S. (1996). Dendroclimatic study in Ural-Siberian Subarctic. Novosibirsk: Nauka Publ., 248 pp. (In Russian).
53. Van Der Schrier G., Barichivich J., Briffa K.R., and Jones P.D. (2013). A scPDSI-based global data set of dry and wet spells for 1901-2009. J. Geophys. Res. Atmos. 118, 4025–4048. doi: 10.1002/jgrd.50355
54. Voropay N.N., Ryazanova A.A. (2023). Changes in hydrothermal conditions in Southern Siberia in 1950–2020 and their relation to largescale circulation processes. Russian Meteorology and Hydrology, 48(10), 897–904. https://doi.org/10.3103/S1068373923100096
55. Wang H., Zuo Z., Qiao L., et al. (2022). Frequency of winter temperature extremes over Siberia dominated by the Atlantic Meridional Overturning Circulation. npj Climate and Atmospheric Science, 5, 84. https://doi.org/10.1038/s41612-022-00307-w
56. Wang X., Xie F., Zhang Z., et al. (2021). Complex network of synchronous climate events in East Asian tree-ring data. Climatic Change, 165, 54. https://doi.org/10.1007/s10584-021-03008-0
57. Wilhite D.A., Glantz M.H. (1985). Understanding the drought phenomenon: The role of definitions. Water International, 10(3), 111–120. https://doi.org/10.1080/02508068508686328
58. Zadonina N.V., Levi K.G. (2008). Chronology of natural and social phenomena in Siberia and Mongolia: A monograph. Irkutsk: Irkutsk State University Press, 759 pp. (In Russian).
Review
For citations:
Sat S.A., Ayurzhanaev A.A., Andreev S.G., Sodnomov B.V. Spatiotemporal variability of palmer drought severity index inferred from long tree-ring chronologies in the Russian and Mongolian parts of the lake Baikal basin. GEOGRAPHY, ENVIRONMENT, SUSTAINABILITY. 2026;19(2):96-106. https://doi.org/10.24057/2071-9388-2026-4381
JATS XML
































