Academic literature on the topic 'Monsoons - India'

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Journal articles on the topic "Monsoons - India"

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RAJ, Y. E. A., R. SURESH, P. V. SANKARAN, and B. AMUDHA. "Seasonal variation of 200 hPa upper tropospheric features over India in relation to performance of Indian southwest and northeast monsoons." MAUSAM 55, no. 2 (2022): 269–80. http://dx.doi.org/10.54302/mausam.v55i2.1082.

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The relation between 200 hPa upper tropospheric parameters such as temperature, zonal and meridional winds over India with the Indian southwest and northeast monsoons has been studied, based on monthly and seasonal upper air data of 14 well-distributed Indian radiosonde stations for the 36 year period 1963-98. It has been found that by and large, positive temperature/height anomalies, negative zonal wind anomalies and northerly position of the sub-tropical ridge during the preceding months/seasons are associated with good southwest/poor northeast monsoons and that complement of the above with
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Tardif, Delphine, Frédéric Fluteau, Yannick Donnadieu, et al. "The origin of Asian monsoons: a modelling perspective." Climate of the Past 16, no. 3 (2020): 847–65. http://dx.doi.org/10.5194/cp-16-847-2020.

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Abstract. The Cenozoic inception and development of the Asian monsoons remain unclear and have generated much debate, as several hypotheses regarding circulation patterns at work in Asia during the Eocene have been proposed in the few last decades. These include (a) the existence of modern-like monsoons since the early Eocene; (b) that of a weak South Asian monsoon (SAM) and little to no East Asian monsoon (EAM); or (c) a prevalence of the Intertropical Convergence Zone (ITCZ) migrations, also referred to as Indonesian–Australian monsoon (I-AM). As SAM and EAM are supposed to have been trigger
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Lim, Young-Kwon, and Kwang-Yul Kim. "ENSO Impact on the Space–Time Evolution of the Regional Asian Summer Monsoons." Journal of Climate 20, no. 11 (2007): 2397–415. http://dx.doi.org/10.1175/jcli4120.1.

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Abstract This study investigates how ENSO affects the space–time evolution of the Asian summer monsoon (ASM) precipitation and synoptic variables on a 5-day resolution over the entire ASM area. Cyclostationary EOF and regression methods were used to investigate the detailed evolution features associated with ENSO during the prominent life cycle of the ASM (21 May–17 September). This ENSO mode is identified as the third largest component (next to the seasonal cycle and the intraseasonal oscillations with a 40–50-day period) of the ASM rainfall variation. The ENSO mode reveals that the individua
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Santhoshkumar, B., N. K. Sathyamoorthy, V. Geethalakshmi, Ga Dheebakaran, K. Boomiraj, and N. Manikandan. "Standardized Precipitation Index Based Drought Assessment over the North Western Zone of Tamil Nadu, India." International Journal of Environment and Climate Change 13, no. 10 (2023): 1–9. http://dx.doi.org/10.9734/ijecc/2023/v13i102612.

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Drought is a natural disaster that tremendously affect the agriculture production and livelihood. Though the Tamil Nadu state is located at peninsular region of India and contributed from both the monsoons, the frequency of drought is high due to vagaries of monsoonal pattern. A study was conducted at Tamil Nadu Agricultural University to assess the drought characteristics across the north western Agro Climatic Zone (ACZ) of Tamil Nadu using Standardized Precipitation Index (SPI) during the past 30 years (1991-2020). The study clearly indicated that the Salem district had high vulnerability to
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Zheng, Yangxing, M. M. Ali, and Mark A. Bourassa. "Contribution of Monthly and Regional Rainfall to the Strength of Indian Summer Monsoon." Monthly Weather Review 144, no. 9 (2016): 3037–55. http://dx.doi.org/10.1175/mwr-d-15-0318.1.

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Indian summer monsoon rainfall (ISMR; June–September) has both temporal and spatial variability causing floods and droughts in different seasons and locations, leading to a strong or weak monsoon. Here, the authors present the contribution of all-India monthly, seasonal, and regional rainfall to the ISMR, with an emphasis on the strong and weak monsoons. Here, regional rainfall is restricted to the seasonal rainfall over four regions defined by the India Meteorological Department (IMD) primarily for the purpose of forecasting regional rainfall: northwest India (NWI), northeast India (NEI), cen
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Chandel, Vikram, and Tejasvi Chauhan. "Attributing Vegetation Recovery During the Indian Summer Monsoon to Climate Drivers in Central India." Ecology, Economy and Society–the INSEE Journal 6, no. 1 (2023): 109–22. http://dx.doi.org/10.37773/ees.v6i1.927.

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Increasing droughts and heat waves as a result of global warming pose a major threat to forests and croplands in India. Monitoring the dynamics of vegetation during a drought and its recovery is essential for the Indian socio-economy and biodiversity. We investigate vegetation recovery from a stressed state in the pre-monsoon (May) period to the end of the monsoon period (September). We then attribute net change during the monsoon period to climate drivers such as temperature, precipitation, and soil moisture. To delineate non-linear interactions, we use an information-theoretic metric to unde
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JENAMANI, RAJENDRA KUMAR, S. R. KALSI, H. R. HATWAR, and S. K. SUBRAMANIAN. "Another deficient monsoon 2004 - A comparison with drought year 2002 and possible causes." MAUSAM 58, no. 2 (2021): 161–76. http://dx.doi.org/10.54302/mausam.v58i2.1199.

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The rainfall over India as a whole during the summer monsoon season of 2004 was deficient with –13% below normal. Earlier in 2002, India has faced another worst situation when large-scale drought occurred and all India rainfall was below –19%. In the present study, we have compared briefly salient observational features of both the monsoons to find out their distinct characteristics. Comparisons show appearance of many similar as well as contrasting features. Though, both seasons were deficient, their dates of onset of monsoon over Kerala were either before or near the normal date. Progress up
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Fasullo, J. "Atmospheric Hydrology of the Anomalous 2002 Indian Summer Monsoon." Monthly Weather Review 133, no. 10 (2005): 2996–3014. http://dx.doi.org/10.1175/mwr3014.1.

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Abstract The 2002 Indian summer monsoon season is unique because of its exceptional weakness, its association with a relatively weak El Niño, and its precedence by over a decade in which ENSO events fail to be associated with significant monsoon anomalies. In this study, atmospheric hydrology during the 2002 summer monsoon and its relationship to monsoon seasons accompanying El Niño events since 1948 are assessed using reanalysis and satellite fields. Strong hydrologic deficits are identified for July and September 2002. During July, the impact of the disturbed Hadley and Walker circulations i
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Guha, Sukanya. "Echoing Tagore’s Love for the Monsoons." ASIAN-EUROPEAN MUSIC RESEARCH JOURNAL 6 (December 4, 2020): 101–4. http://dx.doi.org/10.30819/aemr.6-8.

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In India, Bengal’s most celebrated literary figure, Rabindranath Tagore, was specifically sensitive regarding the various seasons occurring in India. The monsoon and its relation with Tagore’s songs is the main focus of this paper. The monsoon, when Mother Nature spreads her beauty by unravelling her bounty treasures, is richly expressed by Tagore. In the composition for the khanika (poem) ‘Asho nai tumi phalgune’ [you did not come in the spring season] Tagore says: “when I awaited eagerly for your visit in the spring, you didn’t come. Please, don’t make me wait any longer and do come during t
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Babu, J. Madhu, and S. Raja Rao. "Indian Press Coverage of Farmers’ Suicides in Andhra Pradesh: A Content Analysis." IRA-International Journal of Management & Social Sciences (ISSN 2455-2267) 14, no. 2 (2019): 47. http://dx.doi.org/10.21013/jmss.v14.n2.p3.

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<p>India, consisting of 16 percent of world population subsists only on 2.4 percent land resources. Agriculture is the only source of livelihood to the two third of the population which gives employment to 57 percent of the workforce. Agriculture in India is often regarded as gambling with monsoons, because of its almost exclusive dependency on precipitation from monsoons. The failure of monsoons leading to a series of droughts, lack of better prices, exploitation by middlemen, and Gene Modified (GM) seed companies who are selling expensive cotton seeds and fertilizers, all of which have
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Dissertations / Theses on the topic "Monsoons - India"

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Ponton, Camilo. "Aridification of the Indian subcontinent during the Holocene : implications for landscape evolution, sedimentation, carbon cycle, and human civilizations." Thesis, Massachusetts Institute of Technology, 2012. http://hdl.handle.net/1721.1/77787.

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Thesis (Ph. D.)--Joint Program in Oceanography/Applied Ocean Science and Engineering (Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences; and the Woods Hole Oceanographic Institution), 2012.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references.<br>The Indian monsoon affects the livelihood of over one billion people. Despite the importance of climate to society, knowledge of long-term monsoon variability is limited. This thesis provides Holocene records of monsoon variability, using sediment cores from river-dominated margins of
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Stolbova, Veronika. "Indian Summer Monsoon." Doctoral thesis, Humboldt-Universität zu Berlin, Mathematisch-Naturwissenschaftliche Fakultät, 2016. http://dx.doi.org/10.18452/17492.

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Das Ziel dieser Arbeit ist es Geheimnisse des Indischen Monsuns aufzudecken-ein groß-skaliges Klimaphänomen,das mehr als 1,7 Milliarden Menschen stark beeinflußt.Folglich ist das Verständnis der Mechanismen des Indischen Monsuns und seine erfolgreiche Prognose nicht nur eine Frage von größtem Interesse,sondern auch eine bedeutende wissenschaftliche Herausforderung.Der erste Teil dieser Arbeit ist den extremen Niederschlagsereignissen über dem Indischen Subkontinent gewidmet.In dieser Arbeit wurde gezeigt,dass eine Synchronizität zwischen extremen Niederschlagsereignissen in den Eastern Ghats
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Dixit, Yama. "Holocene monsoon variability inferred from paleolake sediments in Northwestern India." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648308.

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Rodwell, Mark John. "Dynamics of the Indian summer monsoon." Thesis, University of Reading, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.333428.

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Sconcia, Brett. "Intraseasonal variability of the Indian Monsoon." Thesis, University of Reading, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.646013.

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The Indian Monsoon is an extremely important and large-scale meteorological phenomenon that occurs with monotonous regularity every year in the northern hemisphere summer. India and the surrounding regions depend on the monsoon's rains which, although averaged over a season are relatively constant, can vary on timescales of days to weeks with devastating economic and social impact. This study was performed in an effort to gain a little more insight in to the intraseasonal variability of the Indian Monsoon. This was done with the help of an extensive observational study using ECMWF reanalysis d
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Ding, Qinghua. "Physical Linkage Between Indian and East Asian Summer Monsoons." Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/6944.

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Observational evidence is presented to show the existence of a boreal summer teleconnection between the Indian summer monsoon (ISM) and East Asian summer monsoon (EASM). Based on station rainfall data, the dominant patterns of variability in monthly and seasonal rainfall over India-East Asia region are investigated mainly through composite analysis. The association between the midlatitude circulation and Indian monsoon rainfall on interannual time scale has also been examined by using 54-year NCEP/NCAR reanalysis data. The major results are as follows: (1) Associated with the year-to-year fluc
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Achuthavarier, Deepthi. "Role of the Indian and Pacific Oceans in the Indian summer monsoon variability." Fairfax, VA : George Mason University, 2009. http://hdl.handle.net/1920/4524.

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Thesis (Ph.D.)--George Mason University, 2009.<br>Vita: p. 179. Thesis director: V. Krishnamurthy. Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Dynamics. Title from PDF t.p. (viewed June 10, 2009). Includes bibliographical references (p. 171-178). Also issued in print.
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Kaushal, Nikita. "High resolution paleo-monsoon records from peninsular Indian speleothems." Thesis, University of Oxford, 2017. https://ora.ox.ac.uk/objects/uuid:ab1ca849-185f-4619-83d9-fffe48e5cd2b.

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The Indian Summer Monsoon is a major component of the global climatic system. Stalagmites have a proven ability to provide information of such monsoon systems. In this thesis, examination of cave records and field work provides a framework of the spatial and temporal distribution of stalagmites in peninsular India. Stable oxygen isotope records from stalagmites are supported by trace element records. An aragonite stalagmite from the west coast of India suggests that changes in growth surface can effect precipitation through time available for dissolved inorganic carbon removal. Calculation of
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Pattnayak, Kanhu Charan. "Indian summer monsoon circulation and precipitation in the warming atmosphere." Thesis, IIT Delhi, 2015. http://localhost:8080/xmlui/handle/12345678/6896.

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Jerstad, Heid Maria. "Weathering relationships : the intra-action of people with climate in Himalayan India." Thesis, University of Edinburgh, 2016. http://hdl.handle.net/1842/23510.

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Weather – cold, wet, hot and windy – pervades life, material and social. So present and obvious as to provide a challenge for research, material though ephemeral too, weather breaks boundaries and refuses categorisation. While night becomes day, the cold season warms up over weeks and annual patterns are changing on a scale of years, practices in the face of weather transitions are themselves shifting. Based on ten months of fieldwork in the small village of Gau in the Pahari Indian Himalayas this thesis interrogates the saliencies and permeations of weather in people’s lives. It investigates
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Books on the topic "Monsoons - India"

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Chatterji, A. K. Monsoons, floods, and cyclones in India. Radiant Publishers, 1991.

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Prokop, Paweł. Wpływ człowieka na środowisko przyrodnicze w klimacie monsunowym północno-wschodnich Indii: Human impact on environment in the monsoonal climate of Northeast India. IGiPZ PAN, 2013.

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Two monsoons: The life and death of Europeans in India. 2nd ed. Duckworth, 1987.

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Laboratory, Oak Ridge National, Cochin University of Science and Technology., and United States. Agency for International Development., eds. Possible vulnerabilities of Cochin, India, to climate change impacts and response strategies to increase resilience. U.S. Agency for International Development, 2003.

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Singh, Nityanand. Determination of onset and withdrawal dates of summer monsoon across India using NCEP/NCAR re-analysis. Indian Institute of Tropical Meteorology, 2010.

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Frater, Alexander. Chasing the monsoon: A modern pilgrimage through India. Holt, 1992.

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ill, Jaeggi Yoshiko, ed. Monsoon afternoon. Peachtree, 2008.

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Frater, Alexander. Chasing the monsoon. Viking, 1990.

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Frater, Alexander. Chasing the monsoon. Penguin Books, 1991.

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Frater, Alexander. Chasing the monsoon. Knopf, 1991.

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Book chapters on the topic "Monsoons - India"

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Saha, Kshudiram. "Monsoon over Southern Asia (Comprising Pakistan, India, Bangladesh, Myanmar and Countries of Southeastern Asia) and Adjoining Indian Ocean (Region – I)." In Tropical Circulation Systems and Monsoons. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-642-03373-5_4.

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Hancock, James F. "Monsoon Islam." In Spices, scents and silk: catalysts of world trade. CABI, 2021. http://dx.doi.org/10.1079/9781789249743.0015.

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Abstract Summarizing how the Ottoman took over the Middle East, the chapters also outlines the boom of the Muslim trade in Europe. Three powerful Muslim empires eventually ringed the Indian Ocean: the Ottomans controlled the Red Sea, the Safavid Dynasty controlled the Persian Gulf route, and the Mughal Empire covered most of India. The chapters also show the flow of the huge Indian Ocean trading network, stating how Muslim communities grew to become trading empires led by powerful sultans who established strong trading by navigating the seas. The terminals of the ocean trade involves: India, Aden, Ormuz, Swahili Coast of Africa, Strait of Malacca and the City of Malacca, Sumatra and Java, Ceylon, and Moluccas. Also, the chapters provide a summary of the ocean trade with Chinese dynasties and other Far East Asian countries.
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Dimri, A. P., and Amulya Chevuturi. "Western Disturbances – Indian Winter Monsoon." In Western Disturbances - An Indian Meteorological Perspective. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-26737-1_4.

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Singh, Pritpal. "Indian Summer Monsoon Rainfall Prediction." In Applications of Soft Computing in Time Series Forecasting. Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-26293-2_7.

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Gupta, Anil K., M. Prakasam, Som Dutt, Peter D. Clift, and R. R. Yadav. "Evolution and Development of the Indian Monsoon." In Geodynamics of the Indian Plate. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-15989-4_14.

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Gao, Youxi, Fumao Yuen, and Ci Li. "Some Characteristics of Plateau Monsoon and Indian SW Monsoon During Summer, 1979." In Proceedings of International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology. American Meteorological Society, 1986. http://dx.doi.org/10.1007/978-1-935704-19-5_3.

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Uddin, Kabir, Mir A. Matin, and Rajesh Bahadur Thapa. "Rapid Flood Mapping Using Multi-temporal SAR Images: An Example from Bangladesh." In Earth Observation Science and Applications for Risk Reduction and Enhanced Resilience in Hindu Kush Himalaya Region. Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-73569-2_10.

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AbstractIn the HKH region, large areas in Afghanistan, Bangladesh, China, India, Myanmar, Nepal, and Pakistan get inundated by floodwater during every rainy season. Among them, Bangladesh has been experiencing record-high floods where four types prevail: flash flood, local rainfall flood, monsoon river flood, and storm-surge flood; and these occur almost every year due to Bangladesh’s unique geographical setting as the most downstream country in the HKH region.
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Slingo, Julia. "The Indian Summer Monsoon and its Variability." In Beyond El Niño. Springer Berlin Heidelberg, 1999. http://dx.doi.org/10.1007/978-3-642-58369-8_5.

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Sarkar, Partha Pratim, Prashanth Janardhan, and Parthajit Roy. "Analysing the Changing Variations of Indian Ocean Dipole (IOD)—Indian Summer Monsoon Rainfall (ISMR) Relationship Across Northeast India." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2022. http://dx.doi.org/10.1007/978-981-19-4055-2_47.

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Kale, Vishwas S. "Geomorphic Effects of Monsoon Floods on Indian Rivers." In Flood Problem and Management in South Asia. Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-017-0137-2_3.

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Conference papers on the topic "Monsoons - India"

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Rushikesh, Satpute, and Khare Kanchan. "Hybrid Blue-Green Infrastructure: Feasibility Study for the State of Maharashtra; India." In International Web Conference in Civil Engineering for a Sustainable Planet. AIJR Publisher, 2021. http://dx.doi.org/10.21467/proceedings.112.20.

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In India, the 2019 monsoon season arrived very late and heavy, following a severe heatwave. This year's monsoons have brought the highest amount of rain in 25 years and with unprecedented spatial variability. In some districts of Maharashtra, higher-than-average rainfall caused massive flooding, which resulted in the submergence of 2 lakh hectares. Whereas remaining states saw the continued drought conditions from monsoon 2018. This unusual monsoon behaviour is considered an example of the impact of climate change and is expected to intensify and worsen over time. The combination of drought fo
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Chowdhury, Piyali, and Manasa Ranjan Behera. "Impact of Climate Modes on Shoreline Evolution: Southwest Coast of India." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61354.

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Coastal geomorphology is a complex phenomenon which is governed by nearshore wave and tidal climate. Change in climate indices (like sea surface temperature, sea level, intensified cyclone activity, among others) and climate modes (like El Nino Southern Oscillation (ENSO), Southern Annular Mode (SAM), Indian Ocean Dipole (IOD)) affect the wave climate and modify many coastal processes thereby altering the geomorphology of shorelines. In countries like India where tropical and sub-tropical cyclones are common, the coastal geomorphology is under constant threat. Coasts are also vulnerable to ant
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Guha, Himadri, and Partha Pratim Biswas. "Monsoon risks for construction sites in India." In 2008 IEEE International Conference on Industrial Engineering and Engineering Management (IEEM). IEEE, 2008. http://dx.doi.org/10.1109/ieem.2008.4738167.

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Shang, Rong, Ronggao Liu, Yang Liu, and Zuo Lu. "Extracting the vegetation phenology of India monsoon forest." In IGARSS 2016 - 2016 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2016. http://dx.doi.org/10.1109/igarss.2016.7729328.

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Umakanth, N., K. Koteswara Rao, K. Lakshmi, M. P. D. Parimala, B. T. P. Madhav, and M. C. Rao. "Pre-monsoon rainfall over Mawsynram region, India during 2020." In ADVANCED MATERIALS AND RADIATION PHYSICS (AMRP-2020): 5th National e-Conference on Advanced Materials and Radiation Physics. AIP Publishing, 2021. http://dx.doi.org/10.1063/5.0052435.

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Mitra, Ashis K., Satya Prakash, D. S. Pai, and A. K. Srivastava. "Evaluation of multi-satellite rainfall products over India during monsoon." In SPIE Asia-Pacific Remote Sensing, edited by Eastwood Im, Raj Kumar, and Song Yang. SPIE, 2016. http://dx.doi.org/10.1117/12.2223311.

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S., Sruthi, and Mrudula G. "Onset of Indian Summer Monsoon: a retrospective analysis." In SPIE Asia-Pacific Remote Sensing, edited by Tiruvalam N. Krishnamurti and Madhavan N. Rajeevan. SPIE, 2016. http://dx.doi.org/10.1117/12.2224019.

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Fatima, Hashmi, H. C. Upadhyaya, and O. P. Sharma. "Impact of carbonaceous aerosols on Indian monsoon rainfall." In SPIE Asia-Pacific Remote Sensing, edited by Tiruvalam N. Krishnamurti, Jhoon Kim, and Takashi Moriyama. SPIE, 2010. http://dx.doi.org/10.1117/12.867030.

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Zhou, 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.

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Abstract It is of great practical importance to understand the variability of the South China Sea (SCS) monsoon on intraseasonal time scales, since the anomalous enhancement of the SCS monsoon may exert serious impacts on the safety of offshore engineering and marine transportation. Our composite analysis shows that the SCS surface wind anomalies are considerably varying with the Madden-Julian Oscillation (MJO) eastward propagation. The SCS summer southwest monsoon tends to be stronger (weaker) in phases 5–8 (1–4) of MJO with the largest positive (negative) wind-speed anomalies when the MJO co
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Srivastava, S., R. Ghoshal, and B. Devaraju. "USE OF GRACE DATA FOR UNDERSTANDING THE INDIAN MONSOON." In 18th Annual Meeting of the Asia Oceania Geosciences Society (AOGS 2021). WORLD SCIENTIFIC, 2022. http://dx.doi.org/10.1142/9789811260100_0050.

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Reports on the topic "Monsoons - India"

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Shroyer, Emily, and James Moum. SST Control by Subsurface Mixing during Indian Ocean Monsoons. Defense Technical Information Center, 2014. http://dx.doi.org/10.21236/ada623418.

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Shroyer, Emily, and James Moum. SST Control by Subsurface Mixing during Indian Ocean Monsoons: 1-yr Pilot Project. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada599181.

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Mahadevan, Amala, and Amit Tandon. Role of the Bay of Bengal for Prediction of Indian Monsoon. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada584875.

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Bala, G. A brief survey on climate change effects on the Indian Monsoon. Office of Scientific and Technical Information (OSTI), 2007. http://dx.doi.org/10.2172/1036853.

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Annamalai, H. Future projection of mean and variability of the Asian Summer Monsoon and Indian Ocean Climate systems. Office of Scientific and Technical Information (OSTI), 2014. http://dx.doi.org/10.2172/1156690.

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Sperber, 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), 1993. http://dx.doi.org/10.2172/10108010.

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Hecht, 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), 2018. http://dx.doi.org/10.2172/1467309.

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Murtugudde, Raghu. Bay of Bengal as the Gateway to Indian Monsoon at Intraseasonal Time-scales: A Regional Coupled Model Study. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada598515.

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Fernando, H. J. ASIRI: Air-Sea Interactions in Northern Indian Ocean (and Its Relation to Monsoonal Dynamics of the Bay of Bengal). Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada590509.

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