Książki na temat „Plateau region”

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1

Boulé, Mary Null. Plateau region: Yakama people. Vashon, WA: Merryant Publishers, 1997.

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2

Boulé, Mary Null. Plateau region: Nez Percé people. Vashon, WA: Merryant Publishers, 1998.

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3

Weaver, H. Dwight. The wilderness underground: Caves of the Ozark plateau. Columbia: University of Missouri Press, 1992.

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4

Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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5

Jetson, Tim. History of the Midlands-Central Plateau region: Printed sources. Hobart, Tas: Centre for Tasmanian Historical Studies, University of Tasmania, 1991.

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6

Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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7

Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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8

Hereford, Richard. Precipitation history of the Colorado Plateau region, 1900-2000. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 2002.

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9

Andreas, Barbara K. The vascular flora of the glaciated Allegheny plateau region of Ohio. Columbus, Ohio: College of Biological Sciences, Ohio State University, 1989.

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10

Johnson, David W. Wildlife of the canyons: Colorado National Monument and the Colorado Plateau region. [Colorado]: Colorado National Monument Association, 1990.

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11

C, Srivastava R. Rainwater harvesting in plateau region of Orissa-potential, prospects, and technology package. Bhubaneswar: Water Technology Centre for Eastern Region, 1998.

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12

Drewes, Harald. Tectonics of the Potwar Plateau region and the development of syntaxes, Punjab, Pakistan. Washington: U.S. G.P.O., 1995.

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13

Legacy on stone: Rock art of the Colorado plateau and four corners region. Boulder, Colo: Johnson Books, 1990.

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14

Cole, Sally J. Legacy on stone: Rock art of the Colorado Plateau and Four Corners Region. Boulder, Colo: Johnson Books, 2008.

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15

China) International Symposium on Environmental Control and Resources Development in China's Loess Plateau Region (1991 Beijing. International Symposium on Environmental Control and Resources Development in China's Loess Plateau Region: Proceedings. Beijing: [Commission for Integrated Survey of Natural Resources, the Chinese Academy of Sciences, 1991.

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16

Outerbridge, William F. The Logan Plateau: A young physiographic region in West Virginia, Kentucky, Virginia, and Tennessee. Washington: U.S. G.P.O., 1987.

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17

Heffernon, Rick. Growth on the Coconino Plateau: Potential impacts of a water pipeline for the region. Tempe, Ariz: Morrison Institute for Public Policy, School of Public Programs, Arizona State University, 2001.

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18

Peoples of the Mambila Plateau and their relations with the Bamnyo region: C.1840-1901. [Nigeria: s.n.], 2008.

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19

R, Schaeffer Kurtis, red. Among Tibetan texts: History and literature of the Himalayan Plateau. Boston: Wisdom Publications, 2001.

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20

Jain, Ajit Kumar. Marketing in an agricultural region: A geographical study of periodic markets in Vidisha Plateau, Madhya Pradesh. New Delhi: Northern Book Centre, 1993.

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21

Larsen, Lotte Melchior. Geology and petrology of the lower Tertiary plateau basalts of the Scoresby Sund region, east Greenland. Copenhagen, Denmark: Grønlands Geologiske Undersøgelse, 1989.

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22

Simelton, Elisabeth. Climate and human impacts on wheat production and land use in the Loess Plateau region, China. Göteborg: Göteborg University, Department of Earth Sciences, Physical Geography, 2007.

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23

Chengfa, Chang, Royal Society (Great Britain) i Zhongguo ke xue yuan, red. The geological evolution of Tibet: Report of the 1985 Royal Society-Academia Sinica Geotraverse of the Qinghai-Xizang Plateau. London: Royal Society, 1988.

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24

Tague, Christina Lee. Evaluation and potential applications of a combined crop productivity and hydrologic model of the Loess Plateau region in China. Ottawa: National Library of Canada, 1993.

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25

Xu, Yingming. Gao yuan mu qu fa zhan yan jiu: Chang Jiang shang you Chuan xi bei li zheng = Research on the development of plateau pastoral region. Beijing Shi: She hui ke xue wen xian chu ban she, 2012.

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26

L, Varnes Katharine, i Geological Survey (U.S.), red. Plays for assessment in Region III, Colorado Plateau and Basin and Range as of October 4, 1993: 1995 National assessment of oil and gas. Denver, Colo: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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27

Tong, Tao. The silk roads of the northern Tibetan plateau during the early Middle Ages (from the Han to Tang Dynasty): As reconstructed from archaeological and written sources. Oxford, England: Archaeopress, 2013.

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28

Steen, O. A. Guide to wetland ecosystems of the very dry montane interior Douglas-fir subzone eastern Fraser Plateau variant (IDFb2) in the Cariboo Forest Region, British Columbia. Victoria, B.C: BC Ministry of Forests and Lands, 1988.

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29

Wang, Mengben. Shanxi Sheng Huangtu Gaoyuan di qu zong he zhi li gui hua yan jiu: Study on the integrated management planning for the Loess Plateau region : Shanxi Province. Wyd. 8. Beijing: Zhongguo lin ye chu ban she, 2009.

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30

Geological Survey (U.S.), red. Processed Landsat 7 Satellite Imagery of the Taos Plateau-San Luis Valley Region, New Mexico and Colorado, U.S. Geological Survey, Open-File Report 2004-1040-B, 2004, (CD-ROM). [S.l: s.n., 2004.

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31

Zizhi, Hu, red. Qing Zang Gaoyuan gao han ren gong cao di sheng chan-sheng tai fan shi: Productive and ecological paradigm of Alpine cultivated grasslands in the region of Qinghai-Tibet Plateau. Beijing: Ke xue chu ban she, 2013.

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32

Mehmet, Bakırcı, i Öz Sinan, red. Doğu Karadeniz yaylalarımız =: Eastern Black Sea Region high plateaus. [Ankara]: Turizm Bakanlığı, Yatırımlar Genel Müdürlüğü Yatırımları Yönlendirme Dairesi Bas̜kanlığı, 1993.

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33

Ding, Shengxi. Qing Zang Gaoyuan zi yuan xing qu yu xin xing cheng zhen hua yan jiu: Yi Chaidamu Pendi wei li = New urbanization research in the resource-oriented region of Qinghai-Tibet Plateau : with Qaidam Basin as an example. Beijing: Zhongguo jing ji chu ban she, 2017.

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34

F, Robertson A. H., Mountrakis D i Geological Society of London, red. Tectonic development of the Eastern Mediterranean region. London: Geological Society, 2006.

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35

E, Clarke Sharon, Bryce Sandra A i Pacific Northwest Research Station (Portland, Or.), red. Hierarchical subdivisions of the Columbia Plateau and Blue Mountains ecoregions, Oregon and Washington. Portland, Or. (333 S.W. First Ave., P.O. Box 3890, Portland 97208): USDA, Forest Service, Pacific Northwest Research Station, 1997.

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36

Blaesing-Thompson, Shawn Renee. Wind erosion on the Columbia Plateau: A mappable solution. [Pullman]: Dept. of Crop and Soil Sciences, Washington State University, 2000.

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37

Plebuch, Raymond O. Potentiometric surface and water quality in the principal aquifer, Mississippian Plateaus region, Kentucky. Louisville, Ky: U.S. Dept. of the Interior, Geological Survey, 1985.

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38

C, Eichelberger J., red. Volcanism and subduction: The Kamchatka region. Washington, DC: American Geophysical Union, 2007.

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39

F, Robertson A. H., Searle M. P i Ries Alison C, red. The geology and tectonics of the Oman Region. London: Geological Society, 1990.

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40

D, Clift P., i Geological Society of London, red. The tectonic and climatic evolution of the Arabian Sea Region. London: Geological Society, 2002.

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41

Macnab, Sandy. A Quarter century of dryland wheat production and marketing: Changes and trends in Oregon's Columbia plateau. [Corvallis, Or.]: Oregon State University Extension Service, 2000.

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42

G, Howell D., i Circum-Pacific Council for Energy and Mineral Resources., red. Tectonostratigraphic terranes of the circum-Pacific region. Houston, Tex., U.S.A: Circum-Pacific Council for Energy and Mineral Resources, 1985.

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43

A, Scrutton R., i Geological Society of London, red. The tectonics, sedimentation, and palaeoceanography of the North Atlantic Region. London: The Geological Society, 1995.

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44

Boule, Mary Null. Yakama People: Plateau Region (Native Americans of North America). Merryant Publishers, 2000.

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45

Schoop, Ulf-Dietrich. The Chalcolithic on the Plateau. Redaktorzy Gregory McMahon i Sharon Steadman. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780195376142.013.0007.

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Streszczenie:
This article outlines the present state of knowledge about the Chalcolithic sequence on the Anatolian plateau and in western Anatolia. Because archaeological knowledge is not represented continuously over the whole area, it will be treated in the context of seven larger regions: the central Anatolian Plain (including Cappadocia, with occasional references to Cilicia), the southwest Anatolian Lake District (a mountainous region around the city of Burdur), the Aegean coast (extending north into the Troad), the area around the Sea of Marmara, the Porsuk region (around the city of Eskişehir), the Black Sea coast (between the cities of Sinop and Trabzon), and north-central Anatolia within the bend of the Kızıl Irmak River. The discussion identifies the main archaeological traditions and their chronological relationships. It also offers an overview of the chronological arguments and contentious issues. All dates are given in calibrated radiocarbon values.
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46

Gibson, A. M., i Henry McCalley. Report on the Coal Measures of the Plateau Region of Alabama. Creative Media Partners, LLC, 2018.

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47

Zhengmianping. An Introduction to Saline Lakes on the Qinghai-Tibet Plateau. Springer, 2012.

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48

Gao, Yanhong, i Deliang Chen. Modeling of Regional Climate over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.591.

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The modeling of climate over the Tibetan Plateau (TP) started with the introduction of Global Climate Models (GCMs) in the 1950s. Since then, GCMs have been developed to simulate atmospheric dynamics and eventually the climate system. As the highest and widest international plateau, the strong orographic forcing caused by the TP and its impact on general circulation rather than regional climate was initially the focus. Later, with growing awareness of the incapability of GCMs to depict regional or local-scale atmospheric processes over the heterogeneous ground, coupled with the importance of this information for local decision-making, regional climate models (RCMs) were established in the 1970s. Dynamic and thermodynamic influences of the TP on the East and South Asia summer monsoon have since been widely investigated by model. Besides the heterogeneity in topography, impacts of land cover heterogeneity and change on regional climate were widely modeled through sensitivity experiments.In recent decades, the TP has experienced a greater warming than the global average and those for similar latitudes. GCMs project a global pattern where the wet gets wetter and the dry gets drier. The climate regime over the TP covers the extreme arid regions from the northwest to the semi-humid region in the southeast. The increased warming over the TP compared to the global average raises a number of questions. What are the regional dryness/wetness changes over the TP? What is the mechanism of the responses of regional changes to global warming? To answer these questions, several dynamical downscaling models (DDMs) using RCMs focusing on the TP have recently been conducted and high-resolution data sets generated. All DDM studies demonstrated that this process-based approach, despite its limitations, can improve understandings of the processes that lead to precipitation on the TP. Observation and global land data assimilation systems both present more wetting in the northwestern arid/semi-arid regions than the southeastern humid/semi-humid regions. The DDM was found to better capture the observed elevation dependent warming over the TP. In addition, the long-term high-resolution climate simulation was found to better capture the spatial pattern of precipitation and P-E (precipitation minus evapotranspiration) changes than the best available global reanalysis. This facilitates new and substantial findings regarding the role of dynamical, thermodynamics, and transient eddies in P-E changes reflected in observed changes in major river basins fed by runoff from the TP. The DDM was found to add value regarding snowfall retrieval, precipitation frequency, and orographic precipitation.Although these advantages in the DDM over the TP are evidenced, there are unavoidable facts to be aware of. Firstly, there are still many discrepancies that exist in the up-to-date models. Any uncertainty in the model’s physics or in the land information from remote sensing and the forcing could result in uncertainties in simulation results. Secondly, the question remains of what is the appropriate resolution for resolving the TP’s heterogeneity. Thirdly, it is a challenge to include human activities in the climate models, although this is deemed necessary for future earth science. All-embracing further efforts are expected to improve regional climate models over the TP.
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49

River Morphodynamics and Stream Ecology of the Qinghai-Tibet Plateau. Taylor & Francis Group, 2016.

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50

Li, Zhiwei, Zhaoyin Wang, Mengzhen Xu i Guo'an Yu. River Morphodynamics and Stream Ecology of the Qinghai-Tibet Plateau. Taylor & Francis Group, 2016.

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