Late Quaternary Climate Variability in the Indian Monsoon Domain

Total Page:16

File Type:pdf, Size:1020Kb

Late Quaternary Climate Variability in the Indian Monsoon Domain LATE QUATERNARY CLIMATE VARIABILITY IN THE INDIAN MONSOON DOMAIN Praveen Kumar Mishra Fachbereich Geowissenschaften, Freie Universität, Berlin December 2014 Late Quaternary climate variability in the Indian monsoon domain (Spät-quartäre klimavariabilität im Gebiet des Indischen monsun) Dissertation zur Erlangung des akademischen Grades Doktor der Naturwissenschaften (Dr. rer. nat.) am Fachbereich Geowissenschaften der Freien Universität Berlin vorgelegt von Praveen Kumar Mishra Berlin, 2014 Als Dissertation angenommen vom Fachbereich Geowissenschaften der Freien Universität Berlin. auf Grund der Gutachten Erstgutachter: Dr. (Habil) Sushma Prasad Zweitgutachter: Prof. Dr. Ulrich Cubasch Datum der Verteidigung: den 07 Mai 2015, Berlin Statement of Authorship The thesis entitled “Late Quaternary climate variability in the Indian monsoon domain” has been submitted for the degree of Doctor in Natural Sciences. I hereby declare that: I have fully acknowledged and referenced the ideas and work of others, whether published or unpublished, in my thesis. This dissertation has not been submitted for the award of any other degree or diploma in any other institution. Praveen Kumar Mishra Berlin, 2014 Acknowledgements I would like to express my deepest gratitude to my advisor, PD Dr. Sushma Prasad, for her excellent guidance, motivation, encouragement during my research. Additionally, I would like to acknowledge Prof. Achim Brauer, for permitting access to laboratory facilities and providing a positive working atmosphere during my stay in the section. I would also like to thank Dr. Peter Dulski, Dr. Birgit Plessen, Dr. Georg Schettler and Mr. Rudolf Naumann for training and permitting me to use their laboratories for sample analysis. Without their help and guidance, it would not have been possible to generate and interpret such a large data set. My grateful thanks are due to other members of the research team, Dr. Birgit Gaye, Dr. A. Anoop, Dr. Philip Menzel, Dr. Elisabeth Dietze, Dr. Stefan Polanski, Dr. Martin Wiesner. My investigations would not been possible without the scientific knowledge and active participation of the Indian partners, especially Prof. A.R. Yousuf, Dr. Arshid Jehangir (Kashmir University), and Prof. N. Basavaiah and Dr. K. Deendayalan (Indian Institute of Geomagnetism, Mumbai). Thanks again to Dr. A. Anoop and Dr. Philip Menzel for their helpful and critical comments on this thesis. In addition, I would like to extend special thanks to Ms. Sylvia Pinkerneil and Ms. Christine Gerschke for helping me in navigating though the complicated administrative matters. I owe additional thanks to Dr. Birgit Plessen and Ms Pinkerneil for their help in laboratory and the fieldwork. I would also like to acknowledge Mr. Dieter Berger, Ms. Gabi Arnold and Mr. Brian Brademann for their help during the laboratory work, and Ms. Ursula Kegel for assisting me during the grain size analysis. My sincere thanks to Mr. Andreas Hendrich for helping me with the beautification of figures and graphs for the manuscripts. I express my warm thanks to Mr. Marcus Günzel and Mr. Matthias Köppl for their help with computer related technical matters. I would also like to thank Arun, Bernhard and the students of Potsdam University, who provided their valuable help during sample processing. My study would not have been possible without Mr. Richard Niederreiter, Mr. Michael Köhler, and Mr. Daniel Niederreiter who were responsible for raising the cores from the Tso Moriri Lake in difficult weather conditions. I thank to all my friends from our ‘Potsdam Gang’ for the unforgettable fun time in Potsdam’s Balzac coffee house’ and enjoyable discussions on various aspect of science, politics and culture. I warmly thank Tarique and Chiranjit for helping me with the editing of the thesis. Additionally, special thanks go to Dharmu, JD bhai, Nishant, Rajak bhai, Sandeep, Somu, Varun, and Vinay for their wonderful and unforgettable friendship, and their encouragement for doing research. Finally, I express my sincere thanks to my father Mr. R.K. Mishra, my mother Mrs. Shila Mishra, and all my family members, for their constant encouragement and support in untold ways. This Ph.D. study has been carried out as part of the research unit “Himalaya: Modern and Past Climates (HIMPAC)” (FOR 1380) which is funded by the “DeutscheForschungsGemeinschaft”. Praveen Kumar Mishra Table of Contents List of Figures ............................................................................................................................................... I List of Tables ............................................................................................................................................... II Abstract ...................................................................................................................................................... III Kurzfassung ................................................................................................................................................ IV Chapter 1: Introduction .............................................................................................................................. 1 1.1. INTRODUCTION .................................................................................................................................... 1 1.1.1. The modern climate system ......................................................................................................... 2 1.1.2. Forcing factors and teleconnections ............................................................................................ 5 1.2. STATE OF THE ART ............................................................................................................................... 8 1.2.1. Literature review: Palaeomonsoon studies .................................................................................. 9 1.3. MOTIVATION AND OBJECTIVES.......................................................................................................... 13 1.4. STUDY AREA ...................................................................................................................................... 15 1.4.1. Tso Moriri Lake, NW Himalaya ............................................................................................... 15 1.4.2. Lonar Lake, central India .......................................................................................................... 16 1.5. ORGANISATION OF THESIS ................................................................................................................. 18 Chapter 2: Limnology and modern sedimentation patterns in high altitude Tso Moriri Lake, NW Himalaya – implications for proxy development ..................................................................................... 20 ABSTRACT ................................................................................................................................................ 20 Chapter 3: Reconstructed late quaternary hydrological changes from Lake Tso Moriri, NW- Himalaya ..................................................................................................................................................... 47 ABSTRACT ................................................................................................................................................ 47 3.1. INTRODUCTION .................................................................................................................................. 48 3.2. STUDY AREA ...................................................................................................................................... 50 3.2.1. Regional climate ........................................................................................................................ 50 3.2.2. Geology ..................................................................................................................................... 50 3.2.3. Hydrology .................................................................................................................................. 50 3.2.4. Modern vegetation ..................................................................................................................... 51 3.3. METHODOLOGY ................................................................................................................................. 51 3.3.1. Coring and core correlation ....................................................................................................... 51 3.3.2. Chronology ................................................................................................................................ 53 3.3.3. Laboratory methods ................................................................................................................... 53 3.4. RESULTS ............................................................................................................................................ 55 3.4.1. Lithology ................................................................................................................................... 55 3.4.2. Radiocarbon dating ................................................................................................................... 56 3.4.3. Geochemistry and mineralogy ................................................................................................... 56 3.4.4. Grain-size distribution ..............................................................................................................
Recommended publications
  • Hydrothermal Alteration at the Lonar Lake Impact Structure, India: Implications for Impact Cratering on Mars
    Meteoritics & Planetary Science 38, Nr 3, 365–381 (2003) Abstract available online at http://meteoritics.org Hydrothermal alteration at the Lonar Lake impact structure, India: Implications for impact cratering on Mars Justin J. HAGERTY* and Horton E. NEWSOM Institute of Meteoritics, Department of Earth & Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA *Corresponding author. E-mail: [email protected] (Received 12 June 2002; revision accepted 20 February 2003) Abstract–The 50,000 year old, 1.8 km diameter Lonar crater is one of only two known terrestrial craters to be emplaced in basaltic target rock (the 65 million year old Deccan Traps). The composition of the Lonar basalts is similar to martian basaltic meteorites, which establishes Lonar as an excellent analogue for similarly sized craters on the surface of Mars. Samples from cores drilled into the Lonar crater floor show that there are basaltic impact breccias that have been altered by post-impact hydrothermal processes to produce an assemblage of secondary alteration minerals. Microprobe data and X-ray diffraction analyses show that the alteration mineral assemblage consists primarily of saponite, with minor celadonite, and carbonate. Thermodynamic modeling and terrestrial volcanic analogues were used to demonstrate that these clay minerals formed at temperatures between 130°C and 200°C. By comparing the Lonar alteration assemblage with alteration at other terrestrial craters, we conclude that the Lonar crater represents a lower size limit for impact-induced hydrothermal activity. Based on these results, we suggest that similarly sized craters on Mars have the potential to form hydrothermal systems, as long as liquid water was present on or near the martian surface.
    [Show full text]
  • Democratic Citizenship in the Heart of Empire Dissertation Presented In
    POLITICAL ECONOMY OF AMERICAN EDUCATION: Democratic Citizenship in the Heart of Empire Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University Thomas Michael Falk B.A., M.A. Graduate Program in Education The Ohio State University Summer, 2012 Committee Members: Bryan Warnick (Chair), Phil Smith, Ann Allen Copyright by Thomas Michael Falk 2012 ABSTRACT Chief among the goals of American education is the cultivation of democratic citizens. Contrary to State catechism delivered through our schools, America was not born a democracy; rather it emerged as a republic with a distinct bias against democracy. Nonetheless we inherit a great demotic heritage. Abolition, the labor struggle, women’s suffrage, and Civil Rights, for example, struck mighty blows against the established political and economic power of the State. State political economies, whether capitalist, socialist, or communist, each express characteristics of a slave society. All feature oppression, exploitation, starvation, and destitution as constitutive elements. In order to survive in our capitalist society, the average person must sell the contents of her life in exchange for a wage. Fundamentally, I challenge the equation of State schooling with public and/or democratic education. Our schools have not historically belonged to a democratic public. Rather, they have been created, funded, and managed by an elite class wielding local, state, and federal government as its executive arms. Schools are economic institutions, serving a division of labor in the reproduction of the larger economy. Rather than the school, our workplaces are the chief educational institutions of our lives.
    [Show full text]
  • Neoglacial Climate Anomalies and the Harappan Metamorphosis 2 3 Authors: 4 5 Liviu Giosan1*, William D
    Clim. Past Discuss., https://doi.org/10.5194/cp-2018-37 Manuscript under review for journal Clim. Past Discussion started: 4 April 2018 c Author(s) 2018. CC BY 4.0 License. 1 Neoglacial Climate Anomalies and the Harappan Metamorphosis 2 3 Authors: 4 5 Liviu Giosan1*, William D. Orsi2,3, Marco Coolen4, Cornelia Wuchter4, 6 Ann G. Dunlea1, Kaustubh Thirumalai5, Samuel E. Munoz1, Peter D. Clift6, 7 Jeffrey P. Donnelly1, Valier Galy7, Dorian Q. Fuller8 8 9 10 Affiliations: 11 12 1Geology & Geophysics, Woods Hole Oceanographic Institution, MA, USA 13 2Department of Earth and Environmental Sciences, Paleontology & Geobiology, Ludwig- 14 Maximilians-Universität München, 80333 Munich, Germany 15 3GeoBio-CenterLMU, Ludwig-Maximilians-Universität München, 80333 Munich, Germany 16 4Curtin University, Perth, Australia 17 5Brown University, Providence, RI, USA 18 6Geology & Geophysics, Louisiana State University, USA 19 8Marine Chemistry & Geochemistry, Woods Hole Oceanographic Institution, MA, USA 20 7Institute of Archaeology, University College London, London, UK 21 22 *Correspondence: [email protected] 23 24 25 26 1 Clim. Past Discuss., https://doi.org/10.5194/cp-2018-37 Manuscript under review for journal Clim. Past Discussion started: 4 April 2018 c Author(s) 2018. CC BY 4.0 License. 27 Abstract: 28 29 Climate exerted constraints on the growth and decline of past human societies but our knowledge 30 of temporal and spatial climatic patterns is often too restricted to address causal connections. At 31 a global scale, the inter-hemispheric thermal balance provides an emergent framework for 32 understanding regional Holocene climate variability. As the thermal balance adjusted to gradual 33 changes in the seasonality of insolation, the Inter-Tropical Convergence Zone migrated 34 southward accompanied by a weakening of the Indian summer monsoon.
    [Show full text]
  • Bugs R Al, No
    ISSN 2230 – 7052 Newsletter of the $WIU4#NNInvertebrate Conservation & Information Network of South Asia (ICINSA) No. 22, MAY 2016 C. Sunil Kumar Photo: CONTENTS Pages Authenc report of Ceresium leucosccum White (Coleoptera: Cerambycidae: Callidiopini) from Pune and Satara in Maharashtra State --- Paripatyadar, S., S. Gaikwad and H.V. Ghate ... 2-3 First sighng of the Apefly Spalgis epeus epeus Westwood, 1851 (Lepidoptera: Lycaenidae: Milenae: Spalgini) from the Garhwal Himalaya --- Sanjay Sondhi ... 4-5 On a collecon of Odonata (Insecta) from Lonar (Crater) Lake and its environs, Buldhana district, Maharashtra, India --- Muhamed Jafer Palot ... 6-9 Occurrence of Phyllodes consobrina Westwood 1848 (Noctuidae: Lepidoptera) from Southern Western Ghats, India and a review of distribuonal records --- Prajith K.K., Anoop Das K.S., Muhamed Jafer Palot and Longying Wen ... 10-11 First Record of Gerosis bhagava Moore 1866 (Lepidoptera: Hesperiidae) from Bangladesh --- Ashis Kumar Daa ... 12 Present status on some common buerflies in Rahara area, West Bengal --- Wrick Chakraborty & Partha P. Biswas ... 13-17 Addions to the Buerfly fauna of Sundarbans Mangrove Forest, Bangladesh --- Ashis Kumar Daa ... 18 Study on buerfly (Papilionoidea) diversity of Bilaspur city --- Shubhada Rahalkar ... 19-23 Bio-ecology of Swallowtail (Lepidoptera:Papilionidae) Buerflies in Gautala Wildlife Sanctuary of Maharashtra India -- Shinde S.S. Nimbalkar R.K. and Muley S.P. ... 24-26 New report of midge gall (Diptera: Cecidomyiidae) on Ziziphus xylopyrus (Retz.) Willd. (Rhamnaceae) from Northern Western Ghats. Mandar N. Datar and R.M. Sharma ... 27 Rapid assessment of buerfly diversity in a ecotone adjoining Bannerghaa Naonal Park, South Bengaluru Alexander R. Avinash K. Phalke S. Manidip M.
    [Show full text]
  • 006-Chapter-3 (30 to 48).Cdr
    CHAPTER – 3 DRAINAGE PATTERN The word 'Drainage' means flow of water. If you look at the physical map of India, you will find that small streams that flows in different areas combine together to form a major river. In the end, these rivers discharge themselves in large water bodies like Lake or Sea or Bay. The water of a region that flows through a river system is called drainage basin. When a highland, e.g., Mountain, separates two neighbouring drainage basin then this type of highland is called 'Water Divide'. The development of any drainage pattern is determined by the topography of that particular region. The rivers of India can be divided into two parts on the basis of land forms: 1. Rivers of Himalayas 2. Peninsular Rivers As these rivers originate in different geographical regions, they are different from each other. Their difference is evident from the following description: DO YOU KNOW? RIVERS OF HIMALAYAS Amazon river basin is the Most of the Himalayan rivers are largest drainage basin of the perennial. Apart from rainfall, these World. rivers continuously receive supply of FIND OUT water, all the year round, by the melting Which river has largest snow on the peaks of the Mountains. drainage basin in India? Rivers like Indus and Brahmaputra originate from Himalayas. These rivers have cut down the Mountains to form gorges during the course of their flow (Fig. 3.1). The rivers originating from Himalayas, right from their origin point to their journey up to the Sea, they perform several functions. On the upper parts of their course they cause massive erosion and carry with them loads of eroded materials like silt, sand, soil, etc.
    [Show full text]
  • Prokaryotic Biodiversity of Lonar Meteorite Crater Soda Lake Sediment and Community Dynamics During Microenvironmental Ph Homeostasis by Metagenomics
    Prokaryotic Biodiversity of Lonar Meteorite Crater Soda Lake Sediment and Community Dynamics During Microenvironmental pH Homeostasis by Metagenomics Dissertation for the award of the degree "Doctor of Philosophy" Ph.D. Division of Mathematics and Natural Sciences of the Georg-August-Universität Göttingen within the doctoral program in Biology of the Georg-August University School of Science (GAUSS) Submitted by Soumya Biswas from Ranchi (India) Göttingen, 2016 Thesis Committee Prof. Dr. Rolf Daniel Department of Genomic and Applied Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany PD Dr. Michael Hoppert Department of General Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Members of the Examination Board Reviewer: Prof. Dr. Rolf Daniel, Department of Genomic and Applied Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Second Reviewer: PD Dr. Michael Hoppert, Department of General Microbiology, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany Further members of the Examination Board: Prof. Dr. Burkhard Morgenstern, Department of Bioinformatics, Institute of Microbiology and Genetics, Faculty of Biology and Psychology, Georg-August-Universität Göttingen, Germany PD Dr. Fabian Commichau, Department of General Microbiology,
    [Show full text]
  • The Curtis L. Ivey Science Center DEDICATED SEPTEMBER 17, 2004
    NON-PROFIT Office of Advancement ORGANIZATION ALUMNI MAGAZINE COLBY-SAWYER Colby-Sawyer College U.S. POSTAGE 541 Main Street PAID New London, NH 03257 LEWISTON, ME PERMIT 82 C LBY-SAWYER CHANGE SERVICE REQUESTED ALUMNI MAGAZINE I NSIDE: FALL/WINTER 2004 The Curtis L. Ivey Science Center DEDICATED SEPTEMBER 17, 2004 F ALL/WINTER 2004 Annual Report Issue EDITOR BOARD OF TRUSTEES David R. Morcom Anne Winton Black ’73, ’75 CLASS NOTES EDITORS Chair Tracey Austin Ye ar of Gaye LaCasce Philip H. Jordan Jr. Vice-Chair CONTRIBUTING WRITERS Tracey Austin Robin L. Mead ’72 the Arts Jeremiah Chila ’04 Executive Secretary Cathy DeShano Ye ar of Nicole Eaton ’06 William S. Berger Donald A. Hasseltine Pamela Stanley Bright ’61 Adam S. Kamras Alice W. Brown Gaye LaCasce Lo-Yi Chan his month marks the launch of the Year of the Arts, a David R. Morcom Timothy C. Coughlin P’00 Tmultifaceted initiative that will bring arts faculty members to meet Kimberly Swick Slover Peter D. Danforth P’83, ’84, GP’02 the Arts Leslie Wright Dow ’57 with groups of alumni and friends around the country. We will host VICE PRESIDENT FOR ADVANCEMENT Stephen W. Ensign gatherings in art museums and galleries in a variety of cities, and Donald A. Hasseltine Eleanor Morrison Goldthwait ’51 are looking forward to engaging hundreds of alumni and friends in Suzanne Simons Hammond ’66 conversations about art, which will be led by our faculty experts. DIRECTOR OF DEVELOPMENT Patricia Driggs Kelsey We also look forward to sharing information about Colby-Sawyer’s Beth Cahill Joyce Juskalian Kolligian ’55 robust arts curriculum.
    [Show full text]
  • Climatic Variability in Western Victoria
    DROUGHTS AND FLOODING RAINS: A FINE-RESOLUTION RECONSTRUCTION OF CLIMATIC VARIABILITY IN WESTERN VICTORIA, AUSTRALIA, OVER THE LAST 1500 YEARS. CAMERON BARR Thesis submitted for the degree of Doctor of Philosophy, Discipline of Geographical and Environmental Studies, University of Adelaide, Australia. 2010 CHAPTER 1 – INTRODUCTION 1.1 Introduction This thesis presents the results of a study examining the short-term (approximately 1500 year) history of climatic change from the south-eastern Australian mainland. In order to achieve this, fossil diatom assemblages from sediment cores retrieved from two crater lakes in western Victoria are examined in fine resolution and interpreted through the application of a diatom-conductivity transfer function developed specifically for use in low salinity lake systems. 1.2 Research context In early November 2006, the then Prime Minister of Australia, John Howard, called an emergency ‘water summit’ with the premiers of the south-eastern states to discuss the impact of the prevailing drought on water availability in the Murray Darling Basin, a key agricultural region for the nation. At this meeting, the attendees were informed that the drought that was afflicting the region was “the worst in 1000 years” (Shanahan and Warren, 2006). This claim proved so startling that it was widely disseminated through the local and national media and was even reported as far away as the United Kingdom (Vidal, 2006). The Prime Minister, however, remained unconvinced of the veracity of the claim because “there are no records [to verify it against]” (Shanahan and Warren, 2006). This brief exchange between the Nation’s leaders and the press highlights the problems faced by water, agricultural, environmental and social planners in Australia.
    [Show full text]
  • Cousin Bette
    HONORÉ DE BALZAC TRANSLATED BY KATHARINE PRESCOTT WORMELEY COUSIN BETTE ROBERTS BROTHERS 3 SOMERSET STREET BOSTON 1888 COPYRIGHT, 1888, BY ROBERTS BROTHERS. University Press JOHN WILSON AND SON, CAMBRIDGE. COUSIN BETTE. CHAPTER I. WHERE DOES NOT PASSION LURK? ABOUT the middle of July, 1838, one of those hackney carriages lately put into circulation along the streets of Paris and called milords was making its way through the rue de l’Université, carrying a fat man of medium height, dressed in the uniform of a captain of the National Guard. Among Parisians, who are thought to be so witty and wise, we may find some who fancy they are infinitely more attractive in uniform than in their ordinary clothes, and who attribute so depraved a taste to the fair sex that they imagine women are favorably impressed by a bear-skin cap and a military equipment. The countenance of this captain, who belonged to the second legion, wore an air of satisfaction with himself which heightened the brilliancy of his ruddy complexion and his somewhat puffy cheeks. A halo of contentment, such as wealth acquired in business is apt to place around the head of a retired shopkeeper, made it easy to guess that he was one of the elect of Paris, an assis- tant-mayor of his arrondissement at the very least. As may be supposed, therefore, the ribbon of the Legion of honor was not absent from his portly breast, which protruded with all the swagger of a Prussian officer. Sitting proudly erect in a corner of the milord, this decorated being let his eyes rove among the pedestrians on the sidewalk, who, in fact, often come in for smiles which are really intended for beautiful absent faces.
    [Show full text]
  • Physico Chemical Analysis of Lonar Lake with Reference to Bacteriological Study
    Kshama S. Khobragade et. al. / International Journal of Modern Sciences and Engineering Technology (IJMSET) ISSN 2349-3755; Available at https://www.ijmset.com Volume 3, Issue 7, 2016, pp.15-22 Physico Chemical analysis of Lonar Lake with reference to Bacteriological Study Dr. Kshama S. Khobragade1 *Vijaykumar B. Pawar2 Associate Professor and Head, Research Scholar Department of Environmental Science, Department of Environmental Science, S.B.E.S. College of Science, Aurangabad S.B.E.S. College of Science, Aurangabad [email protected] [email protected] Abstract The impact origin of the Lonar crater has been well established based on the evidence of shock metamorphosed material. An attempt has been made to evaluate physicochemical qualities of Lonar Lake water. Water samples were analyzed from 2012 to 2013 for seasonal variation in physicochemical qualities of Lonar lake water and revealed that, the water is alkaline (pH 10.5) and characterized by high concentration of Alkalinity (5786 mg/L), Sulphate (67 mg/L), Magnesium (1043 mg/L), Chloride (2816 mg/L) and Dissolved Oxygen (0.03 mg/L). The data indicated that the alkalinity is increased in monsoon and post-monsoon season while decrease in pre-monsoon season. Likewise the chloride and salinity is increased in pre monsoon season while decreased in monsoon and post-monsoon season. As the Lonar Lake is unique in the world for its alkalinity and salinity of the water but its alkalinity, pH and salinity goes on decrease day by day. Hence this World heritage should be preserved for its alkalinity and salinity. Occurrence of few species of algae and fungi indicate the characteristics nature of bio-flora, which needs further investigation and interpretation Keywords: Lonar Crater, Physico-chemical quality.
    [Show full text]
  • Selected Works of Lu Hsun
    7 =-t SELECTED 1{ORKS OF VO L[I ME FOU R Y,.rj\\r^r 1!a- r.-::4i r.ar\. SELECTED WORKS OF LU HSUN VOLUME FOUR i-, :'fir 4\. itr .y 2 Lu Hsun with his wife and son Taken in September 1933 FOREIGN LANGUAGES PRESS PEKING 1960 T EDITOR'S NOTE Translated by Yang Hsien-yi and Gladys Yang 'Ihe essays in this volume come from four collections: Frinqed Literature* and three volumes of Essays of Chieh.-chieh-ting. Fringed Literature, a collection of sixty-one essays written in 1934, was first published in 1936. The thirty- six essays in the first series of Essagrs of Chieh-chieh-ting were also written in 1934, the forty-eight in the second series in 1935, and the thirty-five in the third series in 1936. The three collections of Essays oJ Chieh-chieh-ting were all published in July 1937 after Lu Hsun's death, the first two having been edited by Lu Hsun, the last by his wife Hsu Kuang-ping. Between 1934 and 1936, when the essays in this volume were written, the spearhead of Japanese invasion had struck south from the northeastern provinces to Pe- king and Tientsin. On April 17, 1934, the Japanese imperialists openly declared that China belonged to their sphere of influence. In 1935, Ho Ying-chin signed the Ho-Umezu Agreement whereby the Kuomin- tang government substantially surrendered China's sovereign rights in the provinces of Hopei and Chahar. In November of the same year, the Japanese occupied Inner Mongolia and set up a puppet "autonomous gov- ernment" there.
    [Show full text]
  • Holocene Climatic Changes in the Westerly-Indian Monsoon Realm
    https://doi.org/10.5194/cp-2020-141 Preprint. Discussion started: 17 November 2020 c Author(s) 2020. CC BY 4.0 License. Holocene climatic changes in the Westerly-Indian Monsoon realm and its anthropogenic impact Nicole Burdanowitz1, Tim Rixen1,2, Birgit Gaye1, Kay-Christian Emeis1,3 1Institute for Geology, Universität Hamburg, Bundesstraße 55, 20146 Hamburg, Germany 5 2Leibniz-Zentrum für Marine Tropenforschung (ZMT), Fahrenheitstraße 6, 28359 Bremen, Germany 3Institute of Coastal Research, Helmholtz Center Geesthacht, Max-Planck-Straße 1, 21502 Geesthacht, Germany Correspondence to: Nicole Burdanowitz ([email protected]) Abstract. The Indian Summer Monsoon (ISM) with its rainfall is the lifeline for people living on the Indian subcontinent 10 today and possibly was the driver of the rise and fall of early agricultural societies in the past. Intensity and position of the ISM have shifted in response to orbitally forced thermal land-ocean contrasts. At the northwestern monsoon margins, interactions between the subtropical westerly jet (STWJ) and the ISM constitute a tipping element in the Earth’s climate system, because their non-linear interaction may be a first-order influence on rainfall. We reconstructed marine sea surface temperature (SST), supply of terrestrial material and vegetation changes from a very well-dated sediment core from the 15 northern Arabian Sea to reconstruct the STWJ-ISM interaction. The Holocene record (from 11,000 years) shows a distinct, but gradual, southward displacement of the ISM in the Early to Mid-Holocene, increasingly punctuated by phases of intensified STWJ events that are coeval with interruptions of North Atlantic overturning circulation (Bond events).
    [Show full text]