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Статті в журналах з теми "Monsoons East Asia"
Lu, Mengmeng, Zhiming Kuang, Song Yang, Zhenning Li, and Hanjie Fan. "A Bridging Role of Winter Snow over Northern China and Southern Mongolia in Linking the East Asian Winter and Summer Monsoons." Journal of Climate 33, no. 22 (November 15, 2020): 9849–62. http://dx.doi.org/10.1175/jcli-d-20-0298.1.
Повний текст джерелаChen, Junming, Ping Zhao, Song Yang, Ge Liu, and Xiuji Zhou. "Simulation and Dynamical Prediction of the Summer Asian–Pacific Oscillation and Associated Climate Anomalies by the NCEP CFSv2." Journal of Climate 26, no. 11 (May 31, 2013): 3644–56. http://dx.doi.org/10.1175/jcli-d-12-00368.1.
Повний текст джерелаLiu, Xiaodong, Qingchun Guo, Zhengtang Guo, Zhi-Yong Yin, Buwen Dong, and Robin Smith. "Where were the monsoon regions and arid zones in Asia prior to the Tibetan Plateau uplift?" National Science Review 2, no. 4 (October 26, 2015): 403–16. http://dx.doi.org/10.1093/nsr/nwv068.
Повний текст джерелаTardif, Delphine, Frédéric Fluteau, Yannick Donnadieu, Guillaume Le Hir, Jean-Baptiste Ladant, Pierre Sepulchre, Alexis Licht, Fernando Poblete, and Guillaume Dupont-Nivet. "The origin of Asian monsoons: a modelling perspective." Climate of the Past 16, no. 3 (May 8, 2020): 847–65. http://dx.doi.org/10.5194/cp-16-847-2020.
Повний текст джерелаChiang, J. C. H., W. Kong, C. H. Wu, and D. S. Battisti. "Origins of East Asian Summer Monsoon Seasonality." Journal of Climate 33, no. 18 (September 15, 2020): 7945–65. http://dx.doi.org/10.1175/jcli-d-19-0888.1.
Повний текст джерелаChen, Quanliang, Luyang Xu, and Hongke Cai. "Impact of Stratospheric Sudden Warming on East Asian Winter Monsoons." Advances in Meteorology 2015 (2015): 1–10. http://dx.doi.org/10.1155/2015/640912.
Повний текст джерелаWang, Bin, Michela Biasutti, Michael P. Byrne, Christopher Castro, Chih-Pei Chang, Kerry Cook, Rong Fu, et al. "Monsoons Climate Change Assessment." Bulletin of the American Meteorological Society 102, no. 1 (January 2021): E1—E19. http://dx.doi.org/10.1175/bams-d-19-0335.1.
Повний текст джерелаAbbas, Sohail, Mian Sabir Hussain, Safdar Ali Sherazi, Mareena Khurshid, and Saadia Sultan Wahla. "Connection between the South and East Asian Monsoons: Comparing Summer Monsoon Rainfall of Pakistan and South Korea." International Journal of Economic and Environmental Geology 11, no. 2 (September 24, 2020): 6–11. http://dx.doi.org/10.46660/ijeeg.vol11.iss2.2020.438.
Повний текст джерелаWang, B., LinHo, Yongsheng Zhang, and M.-M. Lu. "Definition of South China Sea Monsoon Onset and Commencement of the East Asia Summer Monsoon*." Journal of Climate 17, no. 4 (February 15, 2004): 699–710. http://dx.doi.org/10.1175/2932.1.
Повний текст джерелаZhang, Lixia, and Tianjun Zhou. "Drought over East Asia: A Review." Journal of Climate 28, no. 8 (April 7, 2015): 3375–99. http://dx.doi.org/10.1175/jcli-d-14-00259.1.
Повний текст джерелаДисертації з теми "Monsoons East Asia"
Ding, Qinghua. "Physical Linkage Between Indian and East Asian Summer Monsoons." Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/6944.
Повний текст джерелаix, 89 leaves
Moriizumi, Jun, Takehisa Ohkuraa, Shigekazu Hirao, Yuki Nono, Hiromi Yamazawa, Yoon-Shin Kim, Qiuju Guo, Hitoshi Mukai, Yasunori Tohjima, and Takao Iida. "Continuous Atmospheric Radon-222 Concentration Observation in East Asia." American Institite of Physics, 2008. http://hdl.handle.net/2237/12040.
Повний текст джерелаHuang, Bo [Verfasser]. "East Asian summer monsoon simulations: dynamical downscaling and seasonal prediction / Bo Huang." Berlin : Freie Universität Berlin, 2017. http://d-nb.info/1138630616/34.
Повний текст джерелаJacobson, Holger. "The East Asian Summer Monsoon : A comparison of present, Holocene and Eemian climate." Thesis, Umeå universitet, Institutionen för ekologi, miljö och geovetenskap, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-88062.
Повний текст джерелаBühring, Christian. "East Asian monsoon variability on orbital and millennial to sub decadal time scales." [S.l. : s.n.], 2001. http://e-diss.uni-kiel.de/diss/d523.pdf.
Повний текст джерелаJunginger, Annett. "East African climate variability on different time scales : the Suguta Valley in the African-Asian Monsoon Domain." Phd thesis, Universität Potsdam, 2011. http://opus.kobv.de/ubp/volltexte/2011/5683/.
Повний текст джерелаMotivation | Die sozialen und ökonomischen Bedürfnisse Ostafrikas sind in erster Linie von der Wasserverfügbarkeit abhängig, welche durch das regelmäßige Einsetzen der Regenzeiten bestimmt wird. Jegliche Veränderungen der Wasserverfügbarkeit innerhalb der Regenzeiten verursachen Hungersnöte, Ausbruch von Krankheiten oder auch Bevölkerungswanderungen. Klärung der Ursachen von Niederschlagsvariabilitäten erfordert die Auswertung von hochauflösenden Kurz- als auch Langzeitanalysen, welche ich in dieser Arbeit durch drei Studien präsentieren werde. 15,000 Jahre - Suguta Valley | Die Hauptstudie dieser Doktorarbeit befasste sich mit dem Verständnis von Feuchtigkeitsschwankungen innerhalb der Afrikanischen Feuchtperiode (AHP, 5.5 - 14.8 ka BP). In dieser Studie präsentiere ich einen hoch-auflösenden Seespiegel Datensatz aus dem abgeschiedenen, unbewohnten Suguta Tal im nördlichen Grabenbruch in Kenia. Das momentan extrem trockene Tal war während der AHP mit einem 300 m tiefen und 2200 km2 großen Paläo-See bedeckt, was aus nur 26% zusätzlichem Niederschlag resultierte. Diese Erhöhung wurde vermutlich aus der Kombination aus erhöhter atmosphärer Feuchteverfügbarkeit infolge erhöhter früh-Holozäner präzessionsgesteuerten Einstrahlung auf der nördlichen Hemisphere sowie der Verschiebung der feuchten Kongo Luftmassengrenze (CAB) ostwärts über das Ostafrikanische und Äthiopische Plateau erreicht als direkte Folge eines erhöhten atmosphärischen Druckgradienten. Abrupte, starkte Seespiegelschwankungen innerhalb der generellen Feuchtphase sind auf geringe Veränderungen in der solaren Ausstrahlung zurückzufühen, welche zu einer Schwächung des Druckgradienten führten und damit den Einfluss der CAB im Untersuchungsgebiet verhinderten zusammen mit einer allgemeinene Reduktion der atmosphärischen Feuchteverfügbarkeit. Das Ende der AHP erfolgte im Gegensatz dazu eher nicht-linear aufgrund des Wechsels zu einem äquatorialen Einstrahlungsmaximum vor 6.5 ka, welches die AHP in Äthiopien und West-Afrika verlängerte. 200 Jahre - Lake Naivasha | Der zweite Teil dieser Arbeit konzentrierte sich auf die Analyse eines Sedimentkern des Naivasha See aus dem zentralen Kenia Rift über die letzten 200 Jahre, einem der wenigen Frischwasserseen in Ostafrika. Die natürliche Klimavariabilität sollte mittels Proxy-Datensätzen von Diatomeen, Transferfunktionen, geochemischen und sedimentologischen Analysen in dieser Studie aufgedeckt werden. Die Ergebnisse zeigten, dass seit Mitte des 20. Jahrhundert der zunehmende Einfluss des Menschen um den Naivasha See zu kultureller Eutrophierung geführt, welche den Einfluss der natürlichen Klimavariabilität auf den See überprägte. Die Gründe liegen in der Zeit, welche von steigender Industrialisierung und deshalb erhöhtem menschlichen Einfluss auf die Proxy-Daten enthaltenden Seen geprägt ist. Die Ergebnisse verdeutlichen die Notwendigkeit von Proxy-Daten aus unbesiedelten Gebieten, wenn man ,reine‘ Daten zur momentanen Debatte über den anthropogen gesteuerten Klimawandel der letzten 100 Jahre beitragen will. 14 Jahre - Ostafrikanisches Rift | Um räumliche Unregelmäßigkeiten in Proxy-Daten von Ostafrika richtig zu verstehen, konzentrierte sich der dritte Teil dieser Arbeit auf die Auswertung von ausschließlich fernerkundlich erworbenen heutigen, täglichen Niederschlagsreihen (1996-2010). Dies erlaubt ein besseres Verständnis über die möglichen klimatischen Einflussmechanismen und die Abschätzung ihres Einflusses auf die Paläo-Variabilität. Die Studie beschäftigt sich mit der Dynamik saisonaler Niederschlagsverteilung innerhalb der Einzugsgebiete von elf Seebecken im Ostafrikanischen Riftsystem, welche oft für Paläo-Klimastudien benutzt werden. Die Studie ergab, dass Niederschläge in angrenzenden Becken tatsächlich höchst unterschiedlich in ihrer Intensität sein können und dabei zwei- bis dreijährigen Niederschlagsmuster folgen oder sogar gegensätzliche Trends zeigen. Die Variabilität der einzelnen Seebecken wird durch die komplexe Wechselwirkung der Topographie, Form, Länge und Höhe des Einzugsgebietes, der relativen Lage im EARS, sowie dem Einfluss und Intensität der ITCZ und CAB bestimmt, welche z.B. abhängig von der Entwicklung besonders starker Tiefdruckgebiet über Indien, Veränderungen der Meeres-oberflächentemperaturen, QBO und dem 11-Jahres Sonnenzyklus sind. Im direkten Vergleich aller untersuchten Monate stellte sich heraus, dass Juli-September die Jahreszeit mit komplexester Niederschlagsvariabilität ist, besonders für die Becken des Ostafrikanischen Plateau, was durch den unregelmäßigen Einfluss der CAB verursacht wird.
Baker, Alexander John. "Lagrangian modelling of precipitation and speleothem proxy oxygen isotope systematics in the East Asian Summer Monsoon region." Thesis, Durham University, 2015. http://etheses.dur.ac.uk/11460/.
Повний текст джерелаYu, Fengling. "Reconstruction of the East Asian monsoon variability since the mid-Holocene from the Pearl River estuary, southern China." Thesis, Durham University, 2009. http://etheses.dur.ac.uk/69/.
Повний текст джерелаYu, Zhaojie. "Quaternary Indian and East Asian monsoon reconstructions and their impacts on weathering and sediment transport to the ocean." Thesis, Université Paris-Saclay (ComUE), 2017. http://www.theses.fr/2017SACLS189.
Повний текст джерелаThe main objective of this PhD study is to reconstruct the evolution of the Asian monsoons during the Quaternary and their impacts on the continental erosion and sedimentary transfers from land to sea by the investigation of sediments cores collected in the Northern Bay of Bengal, the western Philippines Sea and the Arabian Sea. The implemented scientific strategy involves mineralogical (clay size fraction), sedimentological (grain-size laser) and geochemical (⁸⁷Sr/⁸⁶Sr and εNd) analyses in order to establish sedimentary sources, conditions of erosion and transfer of sediments to the Ocean. The analyses of the concentration of Rare Earth Elements (REE) and εNd were also made on seawater and foraminifera samples to better constrain the εNd as a proxy of weathering in a context of strong seasonal variations of sediment discharges by Himalayan rivers. Clay mineralogy and laser grain-size analyses have been conducted on sediments from core MD06-3050 collected on the Benham Rise (Philippines Sea). Siliciclastic grain-size results indicate variations of the relative proportion of three grain-size sub-populations corresponding to eolian dusts (EM2 about 9-11 μm) and Luzon rivers inputs (EM1 about 2-5 μm and EM3 about 19-25 μm). The long-term evolutions of the EM1/EM2 and smectite/(illite+chlorite) ratios permit to reconstruct variations of the contribution of detrital material deriving from the volcanic arc of Luzon and rainfall intensity of this tropical region. At long time scale, periods of intensification of monsoon rainfall on Luzon are associated to a reduction of precipitation on central China. These periods are also associated to an increase of the zonal gradient of sea surface temperatures on the equatorial Pacific Ocean suggesting a strengthening of El Niña conditions. These results highlight for the first time a strong role of the dynamics of the meridian circulation of ENSO on the long-term changes of rainfall of the tropical western Pacific during the Quaternary. In the Arabian Sea, clay mineralogy, siliciclastic grain-size, ⁸⁷Sr/⁸⁶Sr ratio and εNd were analysed on Quaternary sediments of the IODP site U1457. Our results suggest a change in the relative proportions of sediments from the Deccan Trapps (smectite) and the Indus river (mainly illite and chlorite). Variability of sedimentary sources and sediment transport (turbidites activity) to the Indus Fan have been reconstructed and attributed to monsoon rainfall and the sea level variations. The concentrations of REE combined with εNd were analysed on seawater samples collected in June 2012 along a North-South cross section in the Bay of Bengal. We highlighted from normalized REE patterns that the contributions of dissolved REE from the Ganges-Brahmaputra river system was the main source of the dissolved REE of surface waters of the Bay of Bengal, whereas the desorption of lithogenic particles dominate the dissolved REE of the intermediate and deep waters masses. We then revalued the residence time of the dissolved REE in the Bay of Bengal. A comparison of εNd, obtained just before the increase of the Ganges-Brahmaputra river discharge inferred by Indian monsoon rainfall, with the results obtained by Singh and al. (2012) for seawater samples collected after the peak of river discharge, allowed us to highlight for the first time a seasonal variability of seawater εNd of the Bay of Bengal. εNd have been analysed on planktonic foraminiferas of core MD77-176 located at 1375 m water depth to reconstruct for the first time the seawater εNd record of the intermediate waters masses of northern Bay of Bengal for the last 27 kyr. This new seawater εNd record of the Northern Bay of Bengal give us new constrain for this proxy already used to reconstruct past changes of the Himalayan weathering
Payeur-Poirier, Jean-Lionel [Verfasser], and Stefan [Akademischer Betreuer] Peiffer. "Hydrological dynamics of forested catchments as influenced by the East Asian summer monsoon / Jean-Lionel Payeur-Poirier ; Betreuer: Stefan Peiffer." Bayreuth : Universität Bayreuth, 2018. http://d-nb.info/1156326508/34.
Повний текст джерелаКниги з теми "Monsoons East Asia"
Strategic processes in monsoon Asia's economic development. Baltimore: Johns Hopkins University Press, 1993.
Знайти повний текст джерелаCongbin, Fu, Freney J. R, and Stewart J. W. B, eds. Changes in the human-monsoon system of East Asia in the context of global change. Singapore: World Scientific, 2008.
Знайти повний текст джерела-P, Chang C., ed. East Asian monsoon. Hackensack, NJ: World Scientific, 2004.
Знайти повний текст джерелаChang, C.-P. East Asian Monsoon. WORLD SCIENTIFIC, 2004. http://dx.doi.org/10.1142/5482.
Повний текст джерелаLau, William K. M. Impacts of Aerosols on Climate and Weather in the Hindu-Kush-Himalayas-Gangetic Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.590.
Повний текст джерелаFu, Congbin, J. R. Freney, and J. W. B. Stewart. Changes in the Human-Monsoon System of East Asia in the Context of Global Change. WORLD SCIENTIFIC, 2008. http://dx.doi.org/10.1142/6924.
Повний текст джерелаMentz, Steve, ed. A Cultural History of the Sea in the Early Modern Age. Bloomsbury Publishing Plc, 2021. http://dx.doi.org/10.5040/9781474207256.
Повний текст джерелаTouch of Tropical Spice: From Chili Crab to Laksa 75 Easy-To Prepare Dishes from Monsoon Asia. Tuttle Publishing, 2009.
Знайти повний текст джерелаHameed, Saji N. The Indian Ocean Dipole. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.619.
Повний текст джерелаGao, Yanhong, and Deliang Chen. Modeling of Regional Climate over the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.591.
Повний текст джерелаЧастини книг з теми "Monsoons East Asia"
Yihui, Ding. "The Summer Monsoon in East Asia." In Monsoons over China, 1–90. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-015-8302-2_1.
Повний текст джерелаYihui, Ding. "The Winter Monsoon in East Asia." In Monsoons over China, 91–173. Dordrecht: Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-015-8302-2_2.
Повний текст джерелаHancock, James F. "Monsoon Islam." In Spices, scents and silk: catalysts of world trade, 189–205. Wallingford: CABI, 2021. http://dx.doi.org/10.1079/9781789249743.0015.
Повний текст джерелаAn, Zhisheng, Youbin Sun, Weijian Zhou, Weiguo Liu, Xiaoke Qiang, Xulong Wang, Feng Xian, Peng Cheng, and George S. Burr. "Chinese Loess and the East Asian Monsoon." In Late Cenozoic Climate Change in Asia, 23–143. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-7817-7_2.
Повний текст джерелаChin, Mian, Huisheng Bian, Tom Kucsera, Thomas Diehl, Zhining Tao, Dongchul Kim, and Xiaohua Pan. "Connection Between East Asian Air Pollution and Monsoon System." In Air Pollution in Eastern Asia: An Integrated Perspective, 87–103. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-59489-7_5.
Повний текст джерелаUchijima, Zenbei, and Shunji Ohta. "Probable Effects of Climatic Changes on Plant Production of Monsoon Asia." In Climate Change and Plants in East Asia, 13–24. Tokyo: Springer Japan, 1996. http://dx.doi.org/10.1007/978-4-431-66899-2_2.
Повний текст джерелаUchijima, Zenbei, and Shunji Ohta. "Climatic Change Scenarios for Monsoon Asia Based on 2 × CO2-GCM Experiments." In Climate Change and Plants in East Asia, 3–12. Tokyo: Springer Japan, 1996. http://dx.doi.org/10.1007/978-4-431-66899-2_1.
Повний текст джерелаLau, William K. M., Duane E. Waliser, and Huang-Hsiung Hsu. "Intraseasonal variability of the atmosphere–ocean–climate system: East Asian monsoon." In Intraseasonal Variability in the Atmosphere-Ocean Climate System, 73–110. Berlin, Heidelberg: Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-13914-7_3.
Повний текст джерелаClift, Peter D., Graham D. Layne, and Jerzy Blusztajn. "Marine sedimentary evidence for monsoon strengthening, Tibetan uplift and drainage evolution in East Asia." In Continent-Ocean Interactions Within East Asian Marginal Seas, 255–82. Washington, D. C.: American Geophysical Union, 2004. http://dx.doi.org/10.1029/149gm14.
Повний текст джерелаChen, Rong, and Ji Shen. "Reconstructing Mid- to Late Holocene East Asian Monsoon Variability in the Jingpo Lake, Northeastern China." In Earth Surface Processes and Environmental Changes in East Asia, 95–127. Tokyo: Springer Japan, 2015. http://dx.doi.org/10.1007/978-4-431-55540-7_6.
Повний текст джерелаТези доповідей конференцій з теми "Monsoons East Asia"
Goldsmith, Yonaton, Hai Xu, Pratigya J. Polissar, Wallace Broecker, Peter deMenocal, Jianghu Lan, Peng Cheng, Weijian Zhou, and Zhisheng An. "THE OSCILLATING FRINGE OF THE EAST ASIAN MONSOON." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304574.
Повний текст джерелаZhou, Qun, and Lixin Wei. "Impacts of the Madden-Julian Oscillation on South China Sea Monsoon." In ASME 2020 39th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2020. http://dx.doi.org/10.1115/omae2020-19301.
Повний текст джерелаSun, Zhaobo, Chun Li, and Haishan Chen. "Interdecadal variations of East Asia monsoon and its relation with precipitation over North China." In Third International Asia-Pacific Environmental Remote Sensing Remote Sensing of the Atmosphere, Ocean, Environment, and Space, edited by Zhaobo Sun, Fei-Fei Jin, and Toshiki Iwasaki. SPIE, 2003. http://dx.doi.org/10.1117/12.466586.
Повний текст джерелаZeng, Gang, Wei-Chyung Wang, Zhao-bo Sun, and Zhao-hui Lin. "Natural variability of East Asian summer monsoon simulated by NCAR Cam3 model." In SPIE Optical Engineering + Applications, edited by Wei Gao and Thomas J. Jackson. SPIE, 2009. http://dx.doi.org/10.1117/12.825428.
Повний текст джерелаLukens, William E., Jamie R. Vornlocher, Brian A. Schubert, and Cheng Quan. "DISSECTING THE EAST ASIAN MONSOON: SEASONAL RAINFALL PATTERNS FROM LATE OLIGOCENE FOSSIL WOOD." In Joint 69th Annual Southeastern / 55th Annual Northeastern GSA Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020se-344688.
Повний текст джерелаNarayanan, Sunanda, Gokul Vishwanathan, and Mrudula G. "Possible development mechanisms of pre-monsoon thunderstorms over northeast and east India." In SPIE Asia-Pacific Remote Sensing, edited by Tiruvalam N. Krishnamurti and Madhavan N. Rajeevan. SPIE, 2016. http://dx.doi.org/10.1117/12.2223719.
Повний текст джерелаWang, Lijuan, Zhaoyong Guan, Jinhai He, and Jiangjin Lu. "Climatic features of East Asian subtropical summer monsoon trough and its comparison with South China Sea summer monsoon trough." In SPIE Optics + Photonics. SPIE, 2006. http://dx.doi.org/10.1117/12.677341.
Повний текст джерелаXie, Shucheng, Michael Griffiths, Natalie Burls, and Jiayi Lu. "Lipid Proxies of Hydroclimate Driven by Tropical Pacific Ocean in East Asian Monsoon Regions." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.2922.
Повний текст джерелаGao, Qing-jiu, Li-sheng Hao, Jin-zhong Min, and Zhenhe Ren. "Relationship between interdecadal variability of North China summer rainfall, East Asia summer monsoon, and atmospheric circulation anomaly." In Optical Engineering + Applications, edited by Wei Gao and Susan L. Ustin. SPIE, 2007. http://dx.doi.org/10.1117/12.746936.
Повний текст джерелаXiao, Tiangui, Zhaobo Sun, Jingzhong Ming, and Weibin Chen. "Propagation features of wave-packet signal of interdecadal change of the East Asian summer monsoon." In 2010 3rd International Congress on Image and Signal Processing (CISP). IEEE, 2010. http://dx.doi.org/10.1109/cisp.2010.5647810.
Повний текст джерелаЗвіти організацій з теми "Monsoons East Asia"
Chang, C. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada610240.
Повний текст джерелаChang, C. P. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada541660.
Повний текст джерелаChang, C. P. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 2002. http://dx.doi.org/10.21236/ada627716.
Повний текст джерелаChang, C. P. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada629007.
Повний текст джерелаChang, C. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada630003.
Повний текст джерелаChang, C. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630675.
Повний текст джерелаChang, C. P. Monsoon Disturbances Over Southeast and East Asia and the Adjacent Seas. Fort Belvoir, VA: Defense Technical Information Center, August 2001. http://dx.doi.org/10.21236/ada625761.
Повний текст джерелаSperber, K. R., G. L. Potter, J. S. Boyle, and S. Hameed. Simulation of the Indian and East-Asian summer monsoon in the ECMWF model: Sensitivity to horizontal resolution. Office of Scientific and Technical Information (OSTI), November 1993. http://dx.doi.org/10.2172/10108010.
Повний текст джерелаHecht, Matthew, Gennaro D'Angelo, and Darin Comeau. Climate impact of a regional nuclear weapons exchange: Initial consideration of the Indian and East Asian Summer Monsoon. Office of Scientific and Technical Information (OSTI), August 2018. http://dx.doi.org/10.2172/1467309.
Повний текст джерела