Some publications

Abs 13: Finaev A.F. 1994. The potential of atmospheric pollution of Tajikistan territory. Izv. Ac. Sci. Rep. Tadzh. Dept. Sci. Ear., Issue 1, p. 69-74, (russ.).

The review and analysis of physic-and-geographical conditions influencing accumulation of impurity in atmosphere were done. The sketch-map of annual distribution of atmosphere pollution potential on the territory of Tajikistan and sketch-maps of atmospheric pollution distribution in various seasons were calculated.

Abs 14: Finaev A.F., 1994. Vertical profile of diffuse radiation and year motion of the height convection layer. Izv. Ac. Sci. Rep. Tadzh. Dept. Sci. Ear., Issue 3, p. 59-32, (russ.).

Dependence of diffuse radiation vertical profile on optical thickness of atmosphere was investigated. Function of boundary layer height was received and its annual motion was calculated. The height of boundary layer varies from 950 m a.s.l. (in winter) up to 4850 m a.s.l. (in summer).

Abs 17: Finaev A. 1995. Processes of transportation and sedimentation of dust aerosol. In book: Global Analysis, Interpretation, and Modeling: First Science conference 25-29 September 1995, Garmisch-Partenkirchen. IGBP Secretariat of Germany in Berlin. P-22.

Results of aerosol transportation, sedimentation and accumulation modeling in Tajikistan are given.

Abs 20: Finaev A.F. 1999. Climatic Changes in the Mountain Glacier Area of Pamir. In NATO ASI Series I, Vol. 56. Ice Physics in the Natural Environment. (Eds. Wettlaufer/Dash/Untersteiner). Springer-Verlag. Berlin, Heidelberg. 289-294.

Analysis of data allows us to draw some conclusions about climatic changes in Tajikistan and their connection to the changes of the global climate. (a) Annual air temperatures show a steady increase at all levels from 400 to 4000 m (a.s.l.). (b) The rate of air temperature increase on the plain stations is greater than in the high mountains. (c) The vertical gradient of temperature increases with time and leads to increased atmospheric mixing. (d) The cold half of the year warms up more than the warm half. (e) Precipitation increases in mountain areas more than in the valleys. (f) Precipitation increases more in the cold half of the year than in the warm half. (g) In valleys, a reduction in precipitation occurs in May, and all stations show a reduction in June. (h) Climate warming has caused of some of Pamir�s glaciers to recede.

Abs 21: Finaev A.F., Sosin P.M. 1999. Soils with Mediterranean Type of Climate: East Part of Central Asia. 6^th International Meeting on Soils with Mediterranean Type of Climate. 4-9 July 1999. Barcelona. (Ed. J. Bech). University of Barcelona. 415-417.

Abs 28: Finaev A. Transportation and Sedimentation of Dust Aerosol in Tajikistan. In Book: Pamir and Tian Shan: Glacier and Climate Fluctuations during the Pleistocene and Holocene. International Workshop. July 22-23, 2000. Bayreuth, 2000.

Analysis of geographical and climatic data and the results of different researches allowed us to make 3D model of dust particles sedimentation in loess formation region.

Abs 34: Glazirin G.E., Finaev F.A. 2003. The forecast of mountain glaciation change in Western Tajikistan. The future glaciosphere in requirements of varying climate. The workshop of glaciological association. Pushchino, Moscow area, 17-21 may 2002. MGR Moscow. 2003, V 95, p. 102-106.

One of the important glaciological problems is to estimate possible glaciation change in different mountainous countries. It is forced by forecast of rather considerable climate changes. Glaciarization change in three river basins of Western Tajikistan is calculated in proposing report. The calculations were made for two tributaries of Zeravshan River - Matcha River and Fandarya River, and for well-studied Varzob River basin. Selection of these basins was prompted by the fact that they are located on different sides of Hissar Range.

Abs 36: Finaev A.F. 2003. Conditions of water resources formation. In book: Reports Ac. Sci. Rep. Tadzh. Vol. XLVI, Issue 11-12, p. 40-51.

The article describes natural factors of water resources formation, climate and glaciation in Tajikistan. Glaciation change alternatives under the influence of climate changes are examined.

Abs 41: Sosin P.M., Finaev A.F. 2004. Climatic conditions of Mediterranean subtropical soil formation. Archeology and palaeoecology of Eurasia. Novosibirsk: Institute of archeology and ethnography of the Siberian Branch of the Russian Academy of Science, p. 348-350, (russ.).

Conditions of Mediterranean subtropical soil formation in connection with climate change are discussed in the article.

Abs 42: Finaev A.F. 2004. Model of dust aerosol transportation and sedimentation in southern areas of Tajikistan. Archeology and palaeoecology of Eurasia. Novosibirsk: Institute of archeology and ethnography of the Siberian Branch of the Russian Academy of Science, p. 351-358, (russ.).

3D model for calculation of aerosol sediments thickness in the field of loess formation is given. Results of calculations show that the thickest accumulation layer is formed in southern areas and reaches 0.5-0.6 mm/year. Average dust accumulation layer in Tajikistan makes 0.2 mm/year. This value agrees to loess sections records of early Holocene.

Abs 43: Finaev A.F. 2004. Assessment of climatic conditions influence on labour activity of the human. Archeology and palaeoecology Eurasia. Novosibirsk: Institute of archeology and ethnography of the Siberian Branch of the Russian Academy of Science, p. 359-372, (russ.).

The estimation of comfort and labour capacity change in mountain conditions was made in connection with climate change forecast according various models. 4 scenarios of climate change were used: CCC-EQ, UK-TR, GFDL-TR and Had CM2

Abs 45: Finaev A.F. 2004. Climate and glaciation. Water resources of the Central Asia. Dushanbe: Institute of Water Issues, Hydropower Engineering and Ecology, Academy of Sciences, v. 1, � 1. pp. 55-65. (rus.) (370 kb.)

Abs 46: Finaev A.F. 2005. On research of glaciation in the Central Asia. Water resources of the Central Asia. Dushanbe: Institute of Water Issues, Hydropower Engineering and Ecology, Academy of Sciences, � 2. pp. 70-80. (rus). (1114 kb.)

Abs 50: Finaev A., 2009. Review of hydrometeorological observations in Tajikistan for the period of 1990-2005. In book: Joint Publication of UNESCO-IHP and the German National Committee for IHP/HWRP. Selected papers from the Workshop �Assessment of Snow, Glacier and Water Resources in Asia� held in Almaty, Kazakhstan, 28-30 Nov. 2006. edited by Ludwig N. Braun, Wilfried Hagg, Igor V. Severskiy and Gordon Young. IHP/HWRP-BERICHTE, Heft 8. Koblenz. 55-64. (1225 kb.)

Abs 52: Vladimir B. Aizen, Paul A. Mayewski, Elena Aizen, Daniel Joswiak, Arzhan Surazakov, Susan Kaspari, Bijorn Grigholm, Michael Krachler, Mike Handley, Alexander Finaev. 2009. Stable-isotope and trace element time series from Fedchenko glacier (Pamir) snow/firn cores. Journal of Glaciology, Vol. 55, No. 190, 2009. 275-291. (1038 kb.)

Results of the snow--firn sampling analysis are represented in the abstract. The samples were taken in the upper course of Fedchenko glacier at the altitudes of 5365 and 5206 m. above sea-level. Ways of aerosol particles transportation into glacial areas of the Pamir are also discussed.

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� 2005, , Alexander Finaev Studio. F-Lab

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