Relevant bibliographies by topics / Monsoons - India

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  2. Dissertations / Theses
  3. Books
  4. Book chapters
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Academic literature on the topic 'Monsoons - India'

Author: Grafiati
Published: 4 June 2021
Last updated: 6 September 2023

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Journal articles on the topic "Monsoons - India"

1

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 (January 19, 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 poor southwest/good northeast monsoons. The profiles of the above relationship display a double peak in May and September/October. A multiple regression forecast scheme for seasonal forecasting of northeast monsoon rainfall, based on October data has been derived which when tested in an independent sample of 5 years yielded nearly 50% correct forecasts. The southwest monsoon rainfall of India and the northeast monsoon rainfall of Tamil Nadu/Southern parts of India have been shown to share a negative relationship, though the relationship is discordant rather than decisive, which gets defined better when years of deficient southwest monsoon rainfall get excluded. The feature of good Indian northeast monsoon getting preceded by colder upper tropospheric temperatures as shown in the study tie in well with the accepted mechanism of Asian winter monsoon getting intensified due to cold surges from the Siberian High.
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Tardif, 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.

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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 triggered or enhanced primarily by Asian palaeogeographic changes, their possible inception in the very dynamic Eocene palaeogeographic context remains an open question, both in the modelling and field-based communities. We investigate here Eocene Asian climate conditions using the IPSL-CM5A2 (Sepulchre et al., 2019) earth system model and revised palaeogeographies. Our Eocene climate simulation yields atmospheric circulation patterns in Asia substantially different from modern conditions. A large high-pressure area is simulated over the Tethys ocean, which generates intense low tropospheric winds blowing southward along the western flank of the proto-Himalayan–Tibetan plateau (HTP) system. This low-level wind system blocks, to latitudes lower than 10∘ N, the migration of humid and warm air masses coming from the Indian Ocean. This strongly contrasts with the modern SAM, during which equatorial air masses reach a latitude of 20–25∘ N over India and southeastern China. Another specific feature of our Eocene simulation is the widespread subsidence taking place over northern India in the midtroposphere (around 5000 m), preventing deep convective updraught that would transport water vapour up to the condensation level. Both processes lead to the onset of a broad arid region located over northern India and over the HTP. More humid regions of high seasonality in precipitation encircle this arid area, due to the prevalence of the Intertropical Convergence Zone (ITCZ) migrations (or Indonesian–Australian monsoon, I-AM) rather than monsoons. Although the existence of this central arid region may partly result from the specifics of our simulation (model dependence and palaeogeographic uncertainties) and has yet to be confirmed by proxy records, most of the observational evidence for Eocene monsoons are located in the highly seasonal transition zone between the arid area and the more humid surroundings. We thus suggest that a zonal arid climate prevailed over Asia before the initiation of monsoons that most likely occurred following Eocene palaeogeographic changes. Our results also show that precipitation seasonality should be used with caution to infer the presence of a monsoonal circulation and that the collection of new data in this arid area is of paramount importance to allow the debate to move forward.
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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 (June 1, 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 individual regional monsoons over the ASM domain respond to ENSO in a complex manner. 1) Under the El Niño condition, the early monsoon stage over India, the Bay of Bengal, and the Indochina peninsula is characterized by rainfall deficit, along with a delayed monsoon onset by one or two pentads. This is the result of weakened diabatic heating over the Asian continent and meridional pressure gradient over the Indian Ocean, causing a weak low-tropospheric westerly monsoonal flow and the ensuing moisture transport decrease toward the regional monsoon areas. Onsets of the subsequent regional monsoons are delayed successively by this poorly developed ASM system in the early stage. 2) The Walker circulation anomaly persistently induces an enhanced subsidence over the Maritime Continent, resulting in a drought condition over this region for the entire ASM period. 3) The Hadley circulation anomaly linked to the Walker circulation anomaly over the Tropics drives a rising motion over the subtropical western Pacific, resulting in a wetter south China monsoon. The negative sea level pressure anomaly over the subtropical western Pacific associated with this anomalous Hadley circulation provides an unfavorable condition for the moisture transport toward East Asia, causing drier monsoons over north China, Japan, and Korea regions. 4) This negative sea level pressure anomaly intrudes into India, the Bay of Bengal, and the Indochina peninsula during late July and early August, developing a brief wet period over these regions. In contrast, the physical changes including the onset variation and the monsoon strength addressed above are reversed during La Niña events. In reality, the observed ASM rainfall anomaly does not necessarily follow the ENSO-related patterns addressed above because of other impacts contributing to the rainfall variations. Although the impact of ENSO is moderately important, a comparison with other impacts demonstrates that the rainfall variations are controlled more by regional-scale intraseasonal oscillations.
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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 (August 12, 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 drought followed by Dharmapuri and Namakkal districts during the South West Monsoon (SWM), whereas the Namakkal had high vulnerability followed by Salem and Dharmapuri during North East Monsoon (NEM).
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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 (September 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), central India (CI), and south peninsula India (SPIN). In this study, two rainfall datasets provided by IMD are used: 1) all-India monthly and seasonal (June–September) rainfall series for the entire Indian subcontinent as well as seasonal rainfall series for the four homogeneous regions for the period 1901–2013 and 2) the latest daily gridded rainfall data for the period 1951–2014, which is used for assessment at the extent to which the four regions are appropriate for the intended purpose. Rainfall during July–August contributes the most to the total seasonal rainfall, regardless of whether it is a strong or weak monsoon. Although NEI has the maximum area-weighted rainfall, its contribution is the least toward determining a strong or weak monsoon. It is the rainfall in the remaining three regions (NWI, CI, and SPIN) that controls whether an ISMR is strong or weak. Compared to monthly rainfall, regional rainfall dominates the strong or weak rainfall periods.
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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 (January 31, 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 understand the relative association of climate variables with vegetation productivity on a daily scale. We found that pre-monsoon vegetation stress is influenced by soil moisture (r = 0.8, p < 0.01), which is driven by variations in temperature and precipitation. During the monsoons, precipitation contributes to vegetation recovery from pre-monsoon stress through soil moisture recharge while inhibiting vegetation productivity by limiting the amount of radiation available for photosynthesis. Linear regression shows the significant negative dependence of vegetation recovery on precipitation (β = –0.7, p < 0.01) and positive dependence on soil moisture (β = 0.4, p < 0.1) indicating radiation limitation on photosynthesis...
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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 (November 27, 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 to central India was also normal in both the seasons. While Indian Summer Monsoon Rainfall (ISMR) during June was good, a few longest stagnation periods during advancing stage in July of both the years made unexpected delay of monsoon in covering entire India. Rainfall of July also suffered the most in both the seasons with a record lowest ISMR in 2002. Not a single depression formed in 2002 while in 2004, their frequency was less than half of normal. Analysis of other large-scale monthly anomalous ocean and atmospheric conditions over Indo-Pacific region including El-Nino conditions confirms that ENSO and Equatorial Indian Ocean Oscillation or EQUINOO have caused drought in July 2002, but not in July 2004. This is because very high typhoon formation and their recurvature with significantly higher than normal convection over northwest Pacific associated with record lowest ISMR in July, 2002 in contrast to occurrence of deficient ISMR in July 2004 which was associated with few typhoon formation and less convection. Also in 2002, Indian region was happened to fall exactly under the subsidence branch of Walker circulation with ascending branch over the western Pacific in the season in contrast to 2004, when subsidence was observed to be both over large part of western Pacific and adjoining Indian region.
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Fasullo, J. "Atmospheric Hydrology of the Anomalous 2002 Indian Summer Monsoon." Monthly Weather Review 133, no. 10 (October 1, 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 in the African and Indian Ocean region on vertically integrated moisture transport (VIMT) in the Arabian Sea and India is found to be key to the Indian drought. Interhemispheric coherence in satellite-derived surface wind anomalies is also identified. During September, VIMT and surface wind anomalies, both to the east and west of India, contribute to anomalous moisture divergence in India. Bay of Bengal SST and Indian CAPE anomalies are found to act in response to the season’s major break episodes, contrary to other studies that suggest their role as instigators of break periods. The 2002 season is also found to exhibit characteristics that are common to other recent weak monsoons accompanying El Niño, such as strong westerly VIMT anomalies in the western Pacific Ocean and easterly VIMT anomalies in the Arabian Sea. Hydrologic anomalies that distinguish many recent normal monsoon seasons coinciding with El Niño from the El Niño distribution overall are not evident in 2002. In many respects, the 2002 season thus represents a reemergence of the hydrologic anomalies that have accompanied a strong monsoon–ENSO teleconnection over the past 50 yr and may present a challenge for perspectives that suggest a lasting decoupling of the monsoon–ENSO systems.
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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 the full monsoon”. In another of his songs he visualises on a cloudy sunless day, a person’s longing to share his or her deepest treasure of feeling for that particular important person ‘Emon ghonoghor boroshaye’ [in this heavy downpour] (Tagore 2002: 333, song 248). Through these poetic compositions and many more, one may understand the depth in Tagore’s understanding of the human’s emotional details regarding this specific season. The monsoon may also be disastrous. According to Tagore’s a composition ‘Bame rakho bhoyonkori’ [keep aside the destructions] (Tagore 2002: 394, song 58) he describes as well as wishes that the monsoon keeps away the damage or distress from people’s lives. His tunes blend with his words and emotions, not to mention the ragas that are believed to be related with rain that is popular to the Indian subcontinent such as Rag Megh or Rag Mian ki Malhar. These have been affluently used by Tagore to create emotional feelings through his words. He expresses being a philosopher with whom people can find a connection, irrespective of their regional background.
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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 (March 5, 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 led to a series of suicides committed by farmers across India. Farmers' suicides are a complex phenomenon. Since the 1990s farmer suicides in India have made headlines. The journalist Palagummi Sainath highlighted that 17,500 farmers were suicides between 2002 to 2006. The government figures show 14,000 farmers took their own lives in 2011. The total number of farmers’ suicides crossed 3 lakh mark till in 2014. That most suicides occurred in the states of Andhra Pradesh, Maharashtra, Karnataka, Kerala and Punjab. This study seeks to investigate news items on farmers’ suicides in the Indian newspapers. A quantitative content analysis was adopted in this research. This study used two English dailies i.e. The Hindu and The New Indian Express and two Telugu dailies i.e. Eenadu and Andhrajyothi were taken for analysis. It is not a random sample. In this, a purposive sample method was adopted. The selection time period was one year i.e. from January 1, 2015, to December 31, 2015. Keeping in view ten subject categories have been mainly identified for this research. All the data collected were analyzed simple percentage and mean, standard deviation, ANOVA, Chi-square have been used for analysis. </p>
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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.
Cataloged from PDF version of thesis.
Includes bibliographical references.
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 the Bay of Bengal (off the Godavari River) and the Arabian Sea (off the Indus River). Carbon isotopes of terrestrial plant leaf waxes ([delta]¹³Cwax) preserved in sediment provide integrated and regionally extensive records of flora for both sites. For the Godavari River basin the ([delta]¹³Cwax record shows a gradual increase in aridity-adapted vegetation from ~4,000 until 1,700 years ago followed by the persistence of aridity-adapted plants to the present. The oxygen isotopic composition of planktonic foraminifera from this site indicates drought-prone conditions began as early as -3,000 years BP. The aridity record also allowed examination of relationships between hydroclimate and terrestrial carbon discharge to the ocean. Comparison of radiocarbon measurements of sedimentary plant waxes with planktonic foraminifera reveal increasing age offsets starting -4,000 yrs BP, suggesting that increased aridity slows carbon cycling and/or transport rates. At the second site, a seismic survey of the Indus River subaqueous delta describes the morphology and Holocene sedimentation of the Pakistani shelf and identified suitable coring locations for paleoclimate reconstructions. The ([delta]¹³Cwax record shows a stable arid climate over the dry regions of the Indus plain and a terrestrial biome dominated by C₄ vegetation for the last 6,000 years. As the climate became more arid ~4,000 years, sedentary agriculture took hold in central and south India while the urban Harappan civilization collapsed in the already arid Indus basin. This thesis integrates marine and continental records to create regionally extensive paleoenvironmental reconstructions that have implications for landscape evolution, sedimentation, the terrestrial organic carbon cycle, and prehistoric human civilizations in the Indian subcontinent.
by Camilo Ponton.
Ph.D.
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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 und Nord Pakistan Regionen durch das Zusammenspiel zwischen dem indischen Monsun und einem nicht-Monsun-Niederschlagsmuster verursacht wird.Dieses Ergebnis unterstreicht die Bedeutung der Region Nord-Pakistan zur Ableitung der Wechselwirkung zwischen dem indischen Monsun-System und den West-Störungen,und verbessert daher das Verständnis der Kopplung des indischen Monsuns mit den Extratropen.Der zweite Teil der Arbeit befasst sich mit dem Problem der räumlichen und zeitlichen Organisation des abrupten Übergangs auf den indischen Monsun.Hier wird ein neuartiger Mechanismus des räumlich-zeitlichen Übergangs zur Regenperiode vorgeschlagen.Er hat mehrere Vorteile gegenüber bestehenden Erklärungen der Natur des indischen Monsuns:Es beschreibt den abrupten Übergang in einer gewählten Region des indischen Subkontinents sowie die räumliche Ausbreitung und Variabilität des indischen Monsuns beim Einsetzen entlang der Achse des Monsuns.Der dritte Teil dieser Arbeit konzentriert sich auf das Problem der Vorhersagbarkeit des indischen Monsuns.Das vorgeschlagene Verfahren ermöglicht die Vorhersage des Einsetzens und Endens über einen mehr als zwei Wochen bzw.einen Monat früheren Zeitraum im Vergleich zu bisher bekannten Methoden.Schließlich kann die vorgeschlagene Instrumentarium direkt in das bestehende lang-reichweitige Vorhersagesystem für den Monsuns implementiert werden.
The aim of this thesis is to uncover some of the mysteries surrounding the Indian Monsoon - a large-scale climatic phenomenon affecting more than 1.7 billion people. Consequently, understanding the mechanisms of the Indian monsoon and its successful forecasting is not only a question of great interest, but also a significant scientific challenge. The first part of this thesis is devoted to extreme rainfall events over the Indian subcontinent. In this thesis, I have shown that a synchronicity between extreme rainfall events in the Eastern Ghats and North Pakistan regions is caused by the interplay between the Indian Monsoon and a non-monsoonal precipitation pattern driven by the Westerlies - Western Disturbances. This result highlights the importance of the North Pakistan region for inferring the interaction between the Indian Monsoon system and Western Disturbances, and, therefore, improves the understanding of the Indian Monsoon coupling with the extratropics. The second part of this dissertation is concerned with the problem of the spatial and temporal organization of the abrupt transition to the Indian monsoon. Here, I have proposed a novel mechanism of a spatio-temporal transition to monsoon. It has several advantages in comparison to existing explanations of the Indian Monsoon nature: it describes the abrupt transition to monsoon in a chosen region of the Indian subcontinent, as well as the spatial propagation and variability of the Indian Monsoon onset along the axis of advance of monsoon. The third part of this thesis focuses on the problem of predictability of the Indian Monsoon. I have developed a novel method that predicts the onset and withdrawal dates more than two weeks and a month earlier than existing methods, respectively. Finally, the proposed scheme can be directly implemented into the existing long-range forecasting system of the monsoon''s timing.
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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 data and also some modelling with a simple atmospheric model. In order to interpret results, degrees of simplification will be introduced by compositing and averaging processes that betray the complexities of the monsoon system. However, it will be shown that this allows well-defined atmospheric structures to be obtained for what are known as active and break states of the monsoon. Some observational aspects of the active and break monsoon states will be shown, highlighting the major differences between the two states. This will be followed by a series of modelling experiments with increasing sophistication, although remaining very simple. The results of these will show enough consistency with observations to allow an investigation in to the effects of ENSO on the intraseasonal variability of the Indian monsoon.
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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 fluctuation of Indian summer rainfall, a well-organized upper level teleconnection pattern is obvious over the Eurasia continent with two anomalous anticyclonic (cyclonic) circulations in the strong (weak) monsoon year. One center is located over West Tibet, and the other with an equivalent barotropic structure resides in northeast Asia. This teleconnection establishes a linkage between two monsoon systems. (2) Within the summer season from May to September, above mentioned midlatitude teleconnection pattern undergoes a different structure with the strongest intensity in June and August. Hence, depending on the condition of Indian monsoon, the 'window of linkage' between Indian subcontinent rainfall and East Asian monsoon seems to open only in June or August. (3) On the other hand, a global anomalous wavetrain with favored longitudinal phase has been found in the upper and middle troposphere in each summer month. During June and August, this geographically fixed wavetrain characteristic of a circumglobal feature coincides with the ISM-EASM teleconnection. Based on all these observational results, three possible scenarios are proposed to explain the establishment of the teleconnection. And it seems that the upper level climatological westerly jet, Indian monsoon heating and midlatitude stationary wave activity are important factors that control the establishment of the teleconnection. On intraseasonal time scale, simultaneous and lagged correlation statistics have been calculated between height in northern hemisphere and convection over north India. It is found that prior to the breakout of the convection in north India two anomalous ridges have existed over north of Pakistan and northeast Asia, respectively. A plausible mechanism of this interaction between the westerly flow in the midlatitude and Indian monsoon is also briefly discussed.
ix, 89 leaves
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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.
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 empirical partition coefficients from the aragonite stalagmite indicates that U/Ca, Sr/Ca and P/Ca ratios may be paleo-aridity indicators through the process of Prior Aragonite Precipitation. There may also be source and/or temperature control on the partitioning of Sr/Ca into the aragonite stalagmite. These are the first trace element measurements for stalagmites from peninsular India and some of the few available from aragonite stalagmites. The δ18O composition of a calcite stalagmite from central India that grew from 3130 to 2100 years BP is consistent with the hypothesis that δ18O is controlled by air parcel trajectory and amount of rainout between source and cave site. P/Ca and U/Ca records from this stalagmite provide information on past rainfall conditions. Correlation analysis of δ18O, P/Ca and U/Ca indicates that rainfall amount was not the dominant control on δ18O composition at this cave site. Examination of a stalagmite that has diagenetically altered from aragonite to calcite shows that the δ18O system is extremely susceptible to diagenesis. Sr/Ca and U/Ca of the primary aragonite are retained in secondary calcite. Higher Mg/Ca ratios in secondary calcite compared to primary aragonite indicates that diagenetic fluid adds material to the primary carbonate. The variation in U-Th ages are caused by differential addition and losses of U and Th isotopes.
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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 how people intra-act (Barad 2007) with the weather, though practices, infrastructures and relationships with others. My approach argues for the validity of weather as a means by which to learn about socio-material lives. Pahari villagers live and act within the weather that moves around them. They are subject to, but also modify, their thermal environment. Through housing, clothing and tools such as the fire and the fan they affect the impact of the weather as it meets their bodies, but also daily patterns of movement are coloured by weather considerations. This work views weather in relation to health practices (such as refraining from working during the rain so as not to fall ill), for care of others (such as domestic bovines), for house-building and hospitable relationship-building among neighbours, for negotiation of landslide-fraught access roads to elsewhere and for understandings of pollution in the air. This focus on weather is intended to connect dots for people working on climate change, both within and beyond anthropology, and to contribute to discussions in areas including human-animal relations, health and illness and housing.
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Books on the topic "Monsoons - India"

1

Chatterji, A. K. Monsoons, floods, and cyclones in India. New Delhi: 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. Warszawa: IGiPZ PAN, 2013.

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Two monsoons: The life and death of Europeans in India. 2nd ed. London: 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. [Washington, D.C.]: 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. Pune: Indian Institute of Tropical Meteorology, 2010.

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

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

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

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Frater, Alexander. Chasing the monsoon. New Delhi, India: Penguin Books, 1991.

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Frater, Alexander. Chasing the monsoon. New York: 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, 89–122. Berlin, Heidelberg: 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, 189–205. Wallingford: 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, 83–111. Cham: 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, 127–48. Cham: 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, 499–535. Cham: 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, 30–40. Boston, MA: 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, 201–10. Cham: 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, 103–18. Berlin, Heidelberg: 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, 585–98. Singapore: 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, 65–84. Dordrecht: 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 followed by heavy rainfall increases the risk of massive flooding, influence on natural and man-made systems, including infrastructure and agricultural production in flooded and dry regions. Blue-Green Infrastructure (BGI) is an interconnected network of natural and anthropogenic components, including water bodies and green and open spaces, like bio-retention cells, rain barrels, infiltration trenches, and vegetation swales.
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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 anthropogenic factors like offshore structures, harbours, wave farms and other constructional activities along the shoreline. It is thus necessary to understand the evolution of coastlines under the changing climate scenario. The rapidly growing socio-economic development in south-west coast of India has generated the need to investigate the longshore sediment transport (LST) regime in this region under the influence of variable climate factors like the wave characteristics. The presence of numerous river deltas, estuaries and mud banks makes the situation worse especially during the south-west monsoon season (June-September). The investigation on the contemporary evolution of this coastline has not been undertaken and the knowledge of the climate factors that influence the shorelines of the southern tip of India are unknown. This study attempts to understand the temporal dynamics of the longshore sediment transport in this region.
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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 convection is centered in the western Pacific (far western Indian Ocean), suggesting the highest (lowest) probability of the gale over the SCS. The variation of the western Pacific Subtropical High (WPSH), induced by the variations of the local meridional circulation, is shown to play a crucial role in the MJO-SCS summer monsoon linkage. The SCS winter monsoon is also shown to be modulated by the MJO with strengthened (weakened) surface northeasterly in phases 5–6 (1–2). The extra-tropical East Asian trough and East Asian westerly jet associated with the local meridional circulation can well explain the changes of the MJO-SCS winter monsoon relationship. The opposite responses of the wind direction during the same phases of the MJO between summer and winter may be attributed to the discrepancy of meridional circulation related to the wintertime equatorward shift of the MJO convection. The present study indicates that the MJO could be taken into consideration when applying extended-range weather forecast over the SCS as the predictability of the MJO activity is up to 15–20 day currently.
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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"

1

Shroyer, Emily, and James Moum. SST Control by Subsurface Mixing during Indian Ocean Monsoons. Fort Belvoir, VA: Defense Technical Information Center, September 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. Fort Belvoir, VA: Defense Technical Information Center, September 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. Fort Belvoir, VA: Defense Technical Information Center, May 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), February 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), September 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), November 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), August 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. Fort Belvoir, VA: Defense Technical Information Center, September 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). Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada590509.

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