R Graphics Output

Total Page:16

File Type:pdf, Size:1020Kb

R Graphics Output China China LEGEND Previously sampled Malaise trap site Ecoregion Alashan Plateau semi−desert North Tibetan Plateau−Kunlun Mountains alpine desert Altai alpine meadow and tundra Northeast China Plain deciduous forests Altai montane forest and forest steppe Northeast Himalayan subalpine conifer forests Altai steppe and semi−desert Northern Indochina subtropical forests Amur meadow steppe Northern Triangle subtropical forests Bohai Sea saline meadow Northwestern Himalayan alpine shrub and meadows Central China Loess Plateau mixed forests Nujiang Langcang Gorge alpine conifer and mixed forests Central Tibetan Plateau alpine steppe Ordos Plateau steppe Changbai Mountains mixed forests Pamir alpine desert and tundra Changjiang Plain evergreen forests Qaidam Basin semi−desert Da Hinggan−Dzhagdy Mountains conifer forests Qilian Mountains conifer forests Daba Mountains evergreen forests Qilian Mountains subalpine meadows Daurian forest steppe Qin Ling Mountains deciduous forests East Siberian taiga Qionglai−Minshan conifer forests Eastern Gobi desert steppe Rock and Ice Eastern Himalayan alpine shrub and meadows Sichuan Basin evergreen broadleaf forests Eastern Himalayan broadleaf forests South China−Vietnam subtropical evergreen forests Eastern Himalayan subalpine conifer forests Southeast Tibet shrublands and meadows Emin Valley steppe Southern Annamites montane rain forests Guizhou Plateau broadleaf and mixed forests Suiphun−Khanka meadows and forest meadows Hainan Island monsoon rain forests Taklimakan desert Helanshan montane conifer forests Tarim Basin deciduous forests and steppe Hengduan Mountains subalpine conifer forests Tian Shan foothill arid steppe Huang He Plain mixed forests Tian Shan montane conifer forests Jian Nan subtropical evergreen forests Tian Shan montane steppe and meadows Junggar Basin semi−desert Tibetan Plateau alpine shrublands and meadows Western Karakoram−West Tibetan Plateau alpine steppe Himalayan alpine shrub and meadows Manchurian mixed forests Yarlung Zanbo arid steppe Mizoram−Manipur−Kachin rain forests Yellow Sea saline meadow Mongolian−Manchurian grassland Yunnan Plateau subtropical evergreen forests Nenjiang River grassland.
Recommended publications
  • The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands
    The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Christmas, Sakura. 2016. The Cartographic Steppe: Mapping Environment and Ethnicity in Japan's Imperial Borderlands. Doctoral dissertation, Harvard University, Graduate School of Arts & Sciences. Citable link http://nrs.harvard.edu/urn-3:HUL.InstRepos:33840708 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA The Cartographic Steppe: Mapping Environment and Ethnicity in Japan’s Imperial Borderlands A dissertation presented by Sakura Marcelle Christmas to The Department of History in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the subject of History Harvard University Cambridge, Massachusetts August 2016 © 2016 Sakura Marcelle Christmas All rights reserved. Dissertation Advisor: Ian Jared Miller Sakura Marcelle Christmas The Cartographic Steppe: Mapping Environment and Ethnicity in Japan’s Imperial Borderlands ABSTRACT This dissertation traces one of the origins of the autonomous region system in the People’s Republic of China to the Japanese imperial project by focusing on Inner Mongolia in the 1930s. Here, Japanese technocrats demarcated the borderlands through categories of ethnicity and livelihood. At the center of this endeavor was the perceived problem of nomadic decline: the loss of the region’s deep history of transhumance to Chinese agricultural expansion and capitalist extraction.
    [Show full text]
  • Ecosystem Services Changes Between 2000 and 2015 in the Loess Plateau, China: a Response to Ecological Restoration
    RESEARCH ARTICLE Ecosystem services changes between 2000 and 2015 in the Loess Plateau, China: A response to ecological restoration Dan Wu1, Changxin Zou1, Wei Cao2*, Tong Xiao3, Guoli Gong4 1 Nanjing Institute of Environmental Sciences, Ministry of Environmental Protection, Nanjing, China, 2 Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing, China, 3 Satellite Environment Center, Ministry of Environmental Protection, Beijing, China, 4 Shanxi Academy of Environmental Planning, Taiyuan, China a1111111111 a1111111111 * [email protected] a1111111111 a1111111111 a1111111111 Abstract The Loess Plateau of China is one of the most severe soil and water loss areas in the world. Since 1999, the Grain to Green Program (GTGP) has been implemented in the region. This OPEN ACCESS study aimed to analyze spatial and temporal variations of ecosystem services from 2000 to Citation: Wu D, Zou C, Cao W, Xiao T, Gong G 2015 to assess the effects of the GTGP, including carbon sequestration, water regulation, (2019) Ecosystem services changes between 2000 soil conservation and sand fixation. During the study period, the area of forest land and and 2015 in the Loess Plateau, China: A response grassland significantly expanded, while the area of farmland decreased sharply. Ecosystem to ecological restoration. PLoS ONE 14(1): services showed an overall improvement with localized deterioration. Carbon sequestration, e0209483. https://doi.org/10.1371/journal. pone.0209483 water regulation and soil conservation increased substantially. Sand fixation showed a decreasing trend mainly because of decreased wind speeds. There were synergies Editor: Debjani Sihi, Oak Ridge National Laboratory, UNITED STATES between carbon sequestration and water regulation, and tradeoffs between soil conserva- tion and sand fixation.
    [Show full text]
  • Quantifying Trends of Land Change in Qinghai-Tibet Plateau During 2001–2015
    remote sensing Article Quantifying Trends of Land Change in Qinghai-Tibet Plateau during 2001–2015 Chao Wang, Qiong Gao and Mei Yu * Department of Environmental Sciences, University of Puerto Rico, Rio Piedras, San Juan, PR 00936, USA; [email protected] (C.W.); [email protected] (Q.G.) * Correspondence: [email protected]; Tel.: +1-787-764-0000 Received: 1 September 2019; Accepted: 17 October 2019; Published: 20 October 2019 Abstract: The Qinghai-Tibet Plateau (QTP) is among the most sensitive ecosystems to changes in global climate and human activities, and quantifying its consequent change in land-cover land-use (LCLU) is vital for assessing the responses and feedbacks of alpine ecosystems to global climate changes. In this study, we first classified annual LCLU maps from 2001–2015 in QTP from MODIS satellite images, then analyzed the patterns of regional hotspots with significant land changes across QTP, and finally, associated these trends in land change with climate forcing and human activities. The pattern of land changes suggested that forests and closed shrublands experienced substantial expansions in the southeastern mountainous region during 2001–2015 with the expansion of massive meadow loss. Agricultural land abandonment and the conversion by conservation policies existed in QTP, and the newly-reclaimed agricultural land partially offset the loss with the resulting net change of 5.1%. Although the urban area only expanded 586 km2, mainly at the expense of agricultural − land, its rate of change was the largest (41.2%). Surface water exhibited a large expansion of 5866 km2 (10.2%) in the endorheic basins, while mountain glaciers retreated 8894 km2 ( 3.4%) mainly in the − southern and southeastern QTP.
    [Show full text]
  • (Leech, 1890) (Lepidoptera: Hesperiidae) with Description of Female Genitalia and Taxonomic Notes
    © Entomologica Fennica. 31 August 2016 Distribution of Onryza maga (Leech, 1890) (Lepidoptera: Hesperiidae) with description of female genitalia and taxonomic notes Guoxi Xue, Yufei Li, Zihao Liu, Meng Li & Yingdang Ren Xue, G. X., Li, Y.F., Liu, Z. H., Li, M. & Ren, Y.D. 2016: Distribution of Onryza maga (Leech, 1890) (Lepidoptera: Hesperiidae) with description of female geni- talia and taxonomic notes. — Entomol. Fennica 27: 70–76. For more than twenty years, Hainan, Vietnam, Myanmar, Thailand, Malaysia, Singapore and Indonesia have been erroneously reported in Chinese literature as belonging to the distribution range of Onryza maga (Leech 1890). Based upon a careful survey of specimens and relevant literature, these regions are omitted from the known range of this species. Onryza maga maga is found from northeast Guizhou, south Henan and Qinling-Daba Mountains in Shaanxi of China, its oc- currence in Hunan is confirmed. The adults are redescribed and the variability of wing patterns is discussed. Female genitalia are illustrated and described for the first time. Some biological information and an updated distribution map of the species are provided. G. X. Xue & M. Li, School of Food and Bioengineering, Zhengzhou University of Light Industry, No. 5 Dongfeng Road, Zhengzhou, Henan, 450002, P. R. China; Corresponding author’s e-mail: [email protected] Y. F. Li, School of Medicine, Xi’an Jiaotong University, No. 76 Yanta West Road, Xi’an, Shaanxi, 710061, P. R. China Z. H. Liu, School of Physics, University of Science and Technology of China, No. 96 Jinzhai Road, Hefei, Anhui, 230026, P. R. China Y. D.
    [Show full text]
  • Article-Lanzhou
    13 by He Yuanqing, Yao Tandong, Cheng Guodong, and Yang Meixue Climatic records in a firn core from an Alpine temperate glacier on Mt. Yulong, southeastern part of the Tibetan Plateau Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 73000, China. Mt. Yulong is the southernmost glacier-covered area in Asian southwestern monsoon climate. Their total area is 11.61 km2. Eurasia, including China. There are 19 sub-tropical The glaciers resemble a group of flying dragons, giving Mt. Yulong temperate glaciers on the mountain, controlled by the (white dragon) as its name. Many explorers, tourists, poets and scientists have described southwestern monsoon climate. In the summer of 1999, Mt. Yulong from different points of view (Ward, 1924; Wissmann, a firn core, 10.10 m long, extending down to glacier ice, 1937). However, as they were unable to cross the extremely steep was recovered in the accumulation area of the largest mountain slopes and the forested area to the glacier above 4000 m a.s.l., some reported data were not correct. Most of the literature has glacier, Baishui No.1. Periodic variations of climatic focussed on the alpine landscape and the snow scenery, and there are signals above 7.8 m depth were apparent, and net accu- few accounts of the existing glaciers. Ren et al (1957) and Luo and mulation of four years was identified by the annual Yang (1963) first reported the distribution of these glaciers and of the late Pleistocene glacial landforms. To clarify the scale of glacia- oscillations of isotopic and ionic composition.
    [Show full text]
  • Diversity and Geographical Pattern of Altitudinal Belts in the Hengduan Mountains in China
    J. Mt. Sci. (2010) 7: 123–132 DOI: 10.1007/s11629-010-1011-9 Diversity and Geographical Pattern of Altitudinal Belts in the Hengduan Mountains in China YAO Yonghui, ZHANG Baiping*, HAN Fang, and PANG Yu Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China. E-mail: [email protected] * Corresponding author, e-mail: [email protected] © Science Press and Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg 2010 Abstract: This paper analyses the diversity and effect needs further study. In addition, the data spatial pattern of the altitudinal belts in the quality and data accuracy at present also affect to Hengduan Mountains in China. A total of 7 types of some extent the result of quantitative modeling and base belts and 26 types of altitudinal belts are should be improved with RS/GIS in the future. identified in the study region. The main altitudinal belt lines, such as forest line, the upper limit of dark Keywords: Hengduan Mountains; Altitudinal belt coniferous forest and snow line, have similar spectra; Exposure effect; Quadratic model latitudinal and longitudinal spatial patterns, namely, arched quadratic curve model with latitudes and concave quadratic curve model along longitudinal Introduction direction. These patterns can be together called as “Hyperbolic-paraboloid model”, revealing the complexity and speciality of the environment and Globally and generally, the upper and lower ecology in the study region. This result further limits of altitudinal belts vary (increase) from high validates the hypnosis of a common quadratic model latitudes to low latitudes, from continental for spatial pattern of mountain altitudinal belts peripheries to inland areas, and from very humid proposed by the authors.
    [Show full text]
  • Surface Modelling of Human Population Distribution in China
    Ecological Modelling 181 (2005) 461–478 Surface modelling of human population distribution in China Tian Xiang Yuea,∗, Ying An Wanga, Ji Yuan Liua, Shu Peng Chena, Dong Sheng Qiua, Xiang Zheng Denga, Ming Liang Liua, Yong Zhong Tiana, Bian Ping Sub a Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, 917 Building, Datun, Anwai, Beijing 100101, China b College of Science, Xi’an University of Architecture and Technology, Xi’an 710055, China Received 24 March 2003; received in revised form 23 April 2004; accepted 4 June 2004 Abstract On the basis of introducing major data layers corresponding to net primary productivity (NPP), elevation, city distribution and transport infrastructure distribution of China, surface modelling of population distribution (SMPD) is conducted by means of grid generation method. A search radius of 200 km is defined in the process of generating each grid cell. SMPD not only pays attention to the situation of relative elements at the site of generating grid cell itself but also calculates contributions of other grid cells by searching the surrounding environment of the generating grid cell. Human population distribution trend since 1930 in China is analysed. The results show that human population distribution in China has a slanting trend from the eastern region to the western and middle regions of China during the period from 1930 to 2000. Two scenarios in 2015 are developed under two kinds of assumptions. Both scenarios show that the trends of population floating from the western and middle regions to the eastern region of China are very outstanding with urbanization and transport development.
    [Show full text]
  • Preparing the Shaanxi-Qinling Mountains Integrated Ecosystem Management Project (Cofinanced by the Global Environment Facility)
    Technical Assistance Consultant’s Report Project Number: 39321 June 2008 PRC: Preparing the Shaanxi-Qinling Mountains Integrated Ecosystem Management Project (Cofinanced by the Global Environment Facility) Prepared by: ANZDEC Limited Australia For Shaanxi Province Development and Reform Commission This consultant’s report does not necessarily reflect the views of ADB or the Government concerned, and ADB and the Government cannot be held liable for its contents. (For project preparatory technical assistance: All the views expressed herein may not be incorporated into the proposed project’s design. FINAL REPORT SHAANXI QINLING BIODIVERSITY CONSERVATION AND DEMONSTRATION PROJECT PREPARED FOR Shaanxi Provincial Government And the Asian Development Bank ANZDEC LIMITED September 2007 CURRENCY EQUIVALENTS (as at 1 June 2007) Currency Unit – Chinese Yuan {CNY}1.00 = US $0.1308 $1.00 = CNY 7.64 ABBREVIATIONS ADB – Asian Development Bank BAP – Biodiversity Action Plan (of the PRC Government) CAS – Chinese Academy of Sciences CASS – Chinese Academy of Social Sciences CBD – Convention on Biological Diversity CBRC – China Bank Regulatory Commission CDA - Conservation Demonstration Area CNY – Chinese Yuan CO – company CPF – country programming framework CTF – Conservation Trust Fund EA – Executing Agency EFCAs – Ecosystem Function Conservation Areas EIRR – economic internal rate of return EPB – Environmental Protection Bureau EU – European Union FIRR – financial internal rate of return FDI – Foreign Direct Investment FYP – Five-Year Plan FS – Feasibility
    [Show full text]
  • GIS Assessment of the Status of Protected Areas in East Asia
    CIS Assessment of the Status of Protected Areas in East Asia Compiled and edited by J. MacKinnon, Xie Yan, 1. Lysenko, S. Chape, I. May and C. Brown March 2005 IUCN V 9> m The World Conservation Union UNEP WCMC Digitized by the Internet Archive in 20/10 with funding from UNEP-WCMC, Cambridge http://www.archive.org/details/gisassessmentofs05mack GIS Assessment of the Status of Protected Areas in East Asia Compiled and edited by J. MacKinnon, Xie Yan, I. Lysenko, S. Chape, I. May and C. Brown March 2005 UNEP-WCMC IUCN - The World Conservation Union The designation of geographical entities in this book, and the presentation of the material, do not imply the expression of any opinion whatsoever on the part of UNEP, UNEP-WCMC, and IUCN concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. UNEP-WCMC or its collaborators have obtained base data from documented sources believed to be reliable and made all reasonable efforts to ensure the accuracy of the data. UNEP-WCMC does not warrant the accuracy or reliability of the base data and excludes all conditions, warranties, undertakings and terms express or implied whether by statute, common law, trade usage, course of dealings or otherwise (including the fitness of the data for its intended use) to the fullest extent permitted by law. The views expressed in this publication do not necessarily reflect those of UNEP, UNEP-WCMC, and IUCN. Produced by: UNEP World Conservation Monitoring Centre and IUCN, Gland, Switzerland and Cambridge, UK Cffti IUCN UNEP WCMC The World Conservation Union Copyright: © 2005 UNEP World Conservation Monitoring Centre Reproduction of this publication for educational or other non-commercial purposes is authorized without prior written permission from the copyright holder provided the source is fully acknowledged.
    [Show full text]
  • Essd-2020-71.Pdf
    Discussions https://doi.org/10.5194/essd-2020-71 Earth System Preprint. Discussion started: 7 September 2020 Science c Author(s) 2020. CC BY 4.0 License. Open Access Open Data 1 Consolidating the Randolph Glacier Inventory and the Glacier 2 Inventory of China over the Qinghai-Tibetan Plateau and th 3 Investigating Glacier Changes Since the mid-20 Century 4 Xiaowan Liu1,2,3, Zongxue Xu1,2, Hong Yang3,4, Xiuping Li5, Dingzhi Peng1,2 5 1College of Water Sciences, Beijing Normal University, Beijing, 100875, China 6 2Beijiing Key Laboratory of Urban Hydrological Cycle and Sponge City Technology, Beijing, 100875, China 7 3Eawag, Swiss Federal Institute of Aquatic Science and Technology, 8600 Dübendorf, Switzerland 8 4Department of Environmental Science, MGU University of Basel, Petersplatz 1, 4001, Switzerland 9 5Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China 10 Correspondence to: Zongxue Xu ([email protected]) 11 Abstract. Glacier retreat in the Qinghai-Tibetan Plateau (QTP), the ‘third pole of the world’, has attracted the 12 attention of researchers worldwide. Glacier inventories in the 1970s and the 2000s provide valuable information 13 to infer changes in individual glaciers. However, individual glacier volumes are either missing, incomplete or have 14 large errors in these inventories, and thus, the use of these datasets to investigate changes in glaciers in QTP in the 15 past few decades has become a challenge, particularly in the context of climate change. In this study, individual 16 glacier volume data in the Randolph Glacier Inventory version 4.0 (RGI 4.0, 1970s) and the second Glacier 17 Inventory of China (GIC-Ⅱ, 2000s) are recalculated and consolidated using a slope-dependent algorithm based on 18 elevation datasets for the QTP.
    [Show full text]
  • Downloaded from Brill.Com10/07/2021 12:04:04PM Via Free Access © Koninklijke Brill NV, Leiden, 2017
    Amphibia-Reptilia 38 (2017): 517-532 A new moth-preying alpine pit viper species from Qinghai-Tibetan Plateau (Viperidae, Crotalinae) Jingsong Shi1,2,∗, Gang Wang3, Xi’er Chen4, Yihao Fang5,LiDing6, Song Huang7,MianHou8,9, Jun Liu1,2, Pipeng Li9 Abstract. The Sanjiangyuan region of Qinghai-Tibetan Plateau is recognized as a biodiversity hotspot of alpine mammals but a barren area in terms of amphibians and reptiles. Here, we describe a new pit viper species, Gloydius rubromaculatus sp. n. Shi, Li and Liu, 2017 that was discovered in this region, with a brief taxonomic revision of the genus Gloydius.The new species can be distinguished from the other congeneric species by the following characteristics: cardinal crossbands on the back, indistinct canthus rostralis, glossy dorsal scales, colubrid-like oval head shape, irregular small black spots on the head scales, black eyes and high altitude distribution (3300-4770 m above sea level). The mitochondrial phylogenetic reconstruction supported the validity of the new species and furthermore reaffirms that G. intermedius changdaoensis, G. halys cognatus, G. h. caraganus and G. h. stejnegeri should be elevated as full species. Gloydius rubromaculatus sp. n. was found to be insectivorous: preying on moths (Lepidoptera, Noctuidae, Sideridis sp.) in the wild. This unusual diet may be one of the key factors to the survival of this species in such a harsh alpine environment. Keywords: Gloydius rubromaculatus sp. n., insectivorous, new species, Sanjiangyuan region. Introduction leopards (Uncia uncia), wild yaks (Bos grun- niens) and Tibetan antelopes (Pantholops hodg- The Sanjiangyuan region (the Source of Three sonii) (Shen and Tan, 2012).
    [Show full text]
  • The Variations of Land Surface Phenology in Northeast China and Its Responses to Climate Change from 1982 to 2013
    remote sensing Article The Variations of Land Surface Phenology in Northeast China and Its Responses to Climate Change from 1982 to 2013 Jianjun Zhao 1,†, Yanying Wang 1,†, Zhengxiang Zhang 1,*, Hongyan Zhang 1,*, Xiaoyi Guo 1,†, Shan Yu 1,2,†, Wala Du 3,† and Fang Huang 1,† 1 School of Geographical Sciences, Northeast Normal University, Changchun 130024, China; [email protected] (J.Z.); [email protected] (Y.W.); [email protected] (X.G.); [email protected] (S.Y.); [email protected] (F.H.) 2 Inner Mongolia Key Laboratory of Remote Sensing and Geographic Information System, Huhhot 010022, China 3 Ecological and Agricultural Meteorology Center of Inner Mongolia Autonomous Region, Huhhot 010022, China; [email protected] * Correspondence: [email protected] (Z.Z.); [email protected] (H.Z.); Tel./Fax: +86-431-8509-9550 (Z.Z.); +86-431-8509-9213 (H.Z.) † These authors contributed equally to this work. Academic Editors: Petri Pellikka, Lars Eklundh, Alfredo R. Huete and Prasad S. Thenkabail Received: 4 February 2016; Accepted: 4 May 2016; Published: 12 May 2016 Abstract: Northeast China is located at high northern latitudes and is a typical region of relatively high sensitivity to global climate change. Studies of the land surface phenology in Northeast China and its response to climate change are important for understanding global climate change. In this study, the land surface phenology parameters were calculated using the third generation dataset from the Global Inventory Modeling and Mapping Studies (GIMMS 3g) that was collected from 1982 to 2013 were estimated to analyze the variations of the land surface phenology in Northeast China at different scales and to discuss the internal relationships between phenology and climate change.
    [Show full text]