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{"references": ["1. Yu.M.Petrov klimat I Pogoda Samarkand Gidrometeoizdat, 1982.-99 b. 2. T.N.Dolimov, V.I.Troitsky. Evolutionary geology Tashkent: teacher, 2007.-336 b. 3.V.A.Zubakov. Globalnie klimaticheskie sotia neogena Hydrometioizdat, 1990.-197 b. 4. A.A, Abdiyev. Neftigas areas and aquateries of the world. Tashkent: East, 2009,-493 b. 5. M.L.Arushanov. Klimatichesky spectrum planet Zemlya. Tashkent. Uzgidromet, 2010.-160 b. 6. P.Baratov, M.Magnatqulov, A.Gafnikov, the natural geography of Central Asia. Tashkent: Teacher, 2002.-220 b. 7. K.S.Losev klimat: vchera, Segodnya... zavtra I, L.: Hydrometeoisdat, 1985.-174 b. 8. O.V.Nalivkin Paleogeography Sredney Azii. M.- L.: AN USSR, 1936.-205 b. 9. Srednyaya Aziya. Moscow: \u0418\u0437\u0434.AN USSR, 1958.-648 b. 10. S.S.Shuls. Analiz noveyshiy tektoniki I relefa Tyan-Shanya zapiski Vsesoyuzi. Geograficheskogo obtshestva. T.Z. M.: Geografgu, 1948.-316 b. 11. N.A.Yasamanov Manziltno-klimaticheskie uslovia Yura, Mela I paleogena Yuga USSR, M.: Nauka, 1978.-223 b. 12. N.A.Yasamanov drevnia klimati Zemli. L.: Hydrometeoisdat, 1985.-296 b. 13. M.Qoriyev is the natural geography of Central Asia. Tashkent: Teacher, 1968.-334 b. 14. A.V.Gursky, I.V.Kanevskaya, L.F.Ostapovich Osnovnie itogi introduktsii rasteniy v Pamirskom botanicheskom Sadu. Stalinabad SSR, 1953.-97 b. 15. B.P.Alisov B.V.Poltaraus Climatology. Moskovskogo University, 1974.-290 b. 16. E.P.Borisenkov, L.G.Polozova Kolebania klimata za poslednee tisyacheletie Hydrometeoizdat, 1988.-406 b. 17. Rubinstein E. S., Polozova L. G. Sovremennoe izmenenie klimata. - L.: Hydrometeoiedate. -1966-p. 13-24. 18. X.Arakawa Izmeneniya klimata. Hydrometeoisdat, 1975.-112 b. 19. Series Geograficheskaya Tom 2, Izvestia Akademii Nauk USSR, Izdatelstvo \"Nauka\" 1972.-105-107 b. 20. Vestnik MGU Tom 1, Izvestia Akademii Nauk USSR, Izdatelstvo \"Nauka\" 1975.-108-110 b."]}
Objective and reliable indicators are needed to study periodic and general climate changes in Central Asia. In Central Asia, the meteorological network has existed for only 50-80 years, and its data is not enough to solve questions about the climatic changes that interest us and the climate of past years. In the data of Chronicles and other historical documents, only isolated natural phenomena outside the norm, extremely harsh winters and large floods were recorded. This information is long-winded. One of the important objective indicators of the climate of past years is the annual layers of old trees.
Tree, Forest, spruce, Central Asia, pine spruce, climate, garden, mountain, rain, periods, dendrochronology.
Tree, Forest, spruce, Central Asia, pine spruce, climate, garden, mountain, rain, periods, dendrochronology.
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