Дисертації з теми "Asia, Central – Climate"
Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями
Ознайомтеся з топ-15 дисертацій для дослідження на тему "Asia, Central – Climate".
Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.
Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.
Переглядайте дисертації для різних дисциплін та оформлюйте правильно вашу бібліографію.
Crandell, Casey Zepp. "Climate and Conflict in Central Asia: The Effect of Climate Change on the Politics of Central Asia." Thesis, The University of Arizona, 2013. http://hdl.handle.net/10150/297531.
Повний текст джерелаOzdes, Mehmet. "The effect of climate and aerosol on crop production: a case study of central Asia." Thesis, Georgia Institute of Technology, 2012. http://hdl.handle.net/1853/48997.
Повний текст джерелаMirzabaev, Alisher [Verfasser]. "Climate Volatility and Change in Central Asia : Economic Impacts and Adaptation / Alisher Mirzabaev." Bonn : Universitäts- und Landesbibliothek Bonn, 2013. http://d-nb.info/1043057293/34.
Повний текст джерелаXi, Xin. "Examination of mineral dust variability and linkages to climate and land-cover/land-use change over Asian drylands." Diss., Georgia Institute of Technology, 2014. http://hdl.handle.net/1853/53433.
Повний текст джерелаKariyeva, Jahan. "LAND SURFACE PHENOLOGICAL RESPONSES TO LAND USE AND CLIMATE VARIATION IN A CHANGING CENTRAL ASIA." Diss., The University of Arizona, 2010. http://hdl.handle.net/10150/193619.
Повний текст джерелаPanyushkina, Irina, Nurjan Mukhamadiev, Ann Lynch, Nursagim Ashikbaev, Alexis Arizpe, Christopher O’Connor, Danyar Abjanbaev, Gulnaz Mengdіbayeva, and Abay Sagitov. "Wild Apple Growth and Climate Change in Southeast Kazakhstan." MDPI AG, 2017. http://hdl.handle.net/10150/626428.
Повний текст джерелаSu, Ye. "The Impacts of Climate Changeon River Flow and Riparian Vegetation in the Amu Darya River Delta, Central Asia." Thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-74428.
Повний текст джерелаWortmann, Michel S. J. "Integrating glacier dynamics into hydrological modelling : a climate change impact assessment of the data-scarce headwaters of the Tarim River, Central Asia." Thesis, University College London (University of London), 2018. http://discovery.ucl.ac.uk/10052031/.
Повний текст джерелаBougeois, Laurie. "Variation de la saisonnalité paléogène en Asie Centrale : apport d'une géochimie haute résolution sur des coquilles d'huîtres." Thesis, Rennes 1, 2014. http://www.theses.fr/2014REN1S152/document.
Повний текст джерелаThe modern Asian climate is mainly characterized by a monsoonal duality between humid summers in southern and eastern Asia and arid winters in Central Asia resulting in a strong seasonality in terms of precipitation and temperature in these respective regions. Although Neogene monsoonal intensification - mainly attributed to Tibetan plateau uplift - is well established, Paleogene Asian climate is still poorly understood such that the question of how and when this climate duality was established remains open. During Paleogene times, paleoreliefs due to the ongoing Indo-Asia collision and the land-sea distribution were very different compared to modern. Notably, a shallow epicontinental sea (the Proto-Paratethys) covered part of Europe and Central Asia. During the Eocene (-55 to -34 Ma), the Proto-Paratethys retreated westward while high Asian topographies formed. In this peculiar context, this PhD thesis aims to characterize the evolution of high-frequency climatic fluctuations in Central Asia in order to better constrain the seasonality changes associated with sea retreat, topographic uplift or nascent monsoons. We develop a novel approach using a geochemical multi-proxy methodology on oyster shells. Thanks to incremental analyses of elements and isotopes on bivalve shells, we estimate seasonal variations of temperature and salinity in seawater at high resolution. This enables to constrain precisely the annual-scale water and thermal balances and, by applying this technique to successive oyster bearing deposits widely distributed over Central Asia, aims to characterize Central Asian climate evolution. Combining this geochemical approach with a sedimentological and a numerical studies at larger time- and geographic- scale, this PhD thesis is aiming at better understanding the causes of the Eocene regional climate evolution
Törnqvist, Rebecka. "Basin-scale change in water availability and water quality under intensified irrigated agriculture." Doctoral thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-93214.
Повний текст джерелаAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 4: Submitted. Paper 5: Manuscript.
Gallaud, Audrey. "Interaction orogenèse-climat-érosion en Asie Centrale durant le cénozoïque : l'impact de la surrection de la chaîne du Tianshan sur le climat dans le bassin du Junggar." Orléans, 2008. http://www.theses.fr/2008ORLE2061.
Повний текст джерелаMathis, Marie. "Évolution des paléoenvironnements holocènes au Levant (Syrie, Liban) et en Asie Centrale (Kirghizstan) : impacts climatiques et anthropiques." Thesis, Lyon 1, 2015. http://www.theses.fr/2015LYO10001.
Повний текст джерелаThe first sizeable consequences of human activities on the natural environment are thought to have taken place during the Neolithic revolution, at the beginnings of the Holocene, about 10,000 years ago. The aim of this study is to assess the respective role of climate fluctuations and human activities on the evolution of different environmental contexts (coastal, lake and fluvial / swamp) during this interval using sedimentary and palynological records, and hence improve our understanding of Human-Environment-Climate relationships during the Holocene. The study of these different paleoenvironmental settings through the use of both biotic (pollen) and abiotic (sediment geochemistry) markers allow to constrain the temporal development of the first human influences on the natural environment, and to determine their various modes of action (e.g. pastoralism, cultivation). The sequence of environmental changes reconstructed in this study hence highlights profound regional heterogeneities in the response of the studied areas to climatic and anthropic forcing and thus have important implications for our knowledge of the environment-human relationships at the local and regional scales
Gallaud, Audrey. "Interaction Orogenèse - Climat - Erosion en Asie Centrale durant le Cénozoïque : L'impact de la surrection de la chaîne du Tianshan sur le climat dans le bassin du Junggar." Phd thesis, Université d'Orléans, 2008. http://tel.archives-ouvertes.fr/tel-00361593.
Повний текст джерелаInde-Asie. Cette chaîne forme ainsi une barrière naturelle aux courants atmosphériques d'Asie Centrale et sa surrection a dû avoir un impact sur l'évolution climatique durant le Néogène. Son évolution morphologique est contrôlée par la tectonique et le climat, à plusieurs échelles de temps et d'espace. Le Tianshan est donc un objet naturel pour l'étude des interactions Orogenèse-Climat-Erosion. Le piedmont nord du Tianshan est formé de plis d'avant-pays incisés par des rivières, mettant à l'affleurement des séries fluvio-lacustres cénozoïques des bassins de piedmont, issues de l'érosion de
la chaîne. Une étude sédimentologique (faciès, matière organique-MO et minéraux lourds-ML) a été menée trois sites Jingou He, Kuitun He et Ebi Nor, afin de reconstituer les paléoenvironnements depuis 25 Ma. Il a été montré que la composition organique des sédiments n'est pas liée aux environnements sédimentaires. De plus, les palynofaciès exposent des variations climatiques globales, comme les périodes d'aridification connues en Asie Centrale à ~15, 8 et 3 Ma, ainsi que des variations régionales sur le piedmont nord. La confrontation des résultats avec ceux de l'étude du magnétisme des roches permet d'apporter des informations supplémentaires : les variations climatiques sur le piedmont nord seraient dues soit à la tectonique (~20,5; 15,5; 11,5 et 4,5 Ma), soit au climat (~20,5; ~17,5; ~13,8; ~9-8,8; ~4,5 et ~1,2 Ma).
L'étude sédimentaire des séries néogènes du bassin du Junggar révèle que 1) les palynofaciès permettent de décrire l'évolution des environnements, en terme de degré d'humidité/aridité, cela malgré les faibles contenus organiques, 2) la confrontation avec d'autres paramètres permet de proposer une origine tectonique ou climatique aux changements environnementaux, 3) la corrélation entre les 3 sites d'étude montre que ces variations sont au moins d'échelle régionale.
Sorrel, Philippe. "The Aral Sea : a palaeoclimate archive." Phd thesis, [S.l.] : [s.n.], 2006. http://deposit.ddb.de/cgi-bin/dokserv?idn=981212832.
Повний текст джерелаBinternagel, Norbert. "Adaptation to natural hazards in Central Sulawesi, Indonesia - strategies of rural households." Doctoral thesis, 2010. http://hdl.handle.net/11858/00-1735-0000-0006-B2F8-C.
Повний текст джерела