Annex II (Sub-Report) Supplementary Information in the Field of Carbon
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Review Statement of World Biosphere Reserve [ July 2013 ]
Review Statement of World Biosphere Reserve [ July 2013 ] Prefeace According to the Resolution 28 C/2.4 on Statutory Framework of MAB (Man and Biosphere) Program passed on the 28th session of the UNESCO General Conference, Article 4 has been clearly identified as the criteria which shall be followed by biosphere reserves. In addition, it is stipulated in Article 9 that a Decennium Review shall be conducted on the world biosphere reserve every a decade, this Review shall be based on the report prepared by the relevant authority; the Review result shall be submitted to the relevant national secretariat. The related text of Statutory Framework is attached in Annex 3. This Review Statement will be helpful for each country preparing national reports and update data as stipulated in Article 9, and the secretariat timely accessing to data associated with the biosphere reserve. This Statement shall contribute to the inspection of MAB ICC on the biosphere reserve, and judge whether it can meet all criteria mentioned in Article 9 of the Legal Framework, especially three major functions. It shall be noted that is required to specify how the biosphere reserve achieves the various criteria in the last part of the Statement (Criteria and Progress). The information from Decennium Review will be used by UNESCO for the following purposes: (a) Inspection of the relevant autorities of International Advisory Committee and MAB ICC on the biosphere reserve; and (b) the world's information system, especially the UNESCO's MAB network and publications, so as to promote communication among people concerned the world biosphere reserve and influence each other. -
Seasonal Concentration Distribution of PM1.0 and PM2.5 and a Risk
www.nature.com/scientificreports OPEN Seasonal concentration distribution of PM1.0 and PM2.5 and a risk assessment of bound trace metals in Harbin, China: Efect of the species distribution of heavy metals and heat supply Kun Wang1, Weiye Wang1, Lili Li1, Jianju Li1, Liangliang Wei1 ✉ , Wanqiu Chi1, Lijing Hong1,2, Qingliang Zhao1 & Junqiu Jiang1 To clarify the potential carcinogenic/noncarcinogenic risk posed by particulate matter (PM) in Harbin, a city in China with the typical heat supply, the concentrations of PM1.0 and PM2.5 were analyzed from Nov. 2014 to Nov. 2015, and the compositions of heavy metals and water-soluble ions (WSIs) were determined. The continuous heat supply from October to April led to serious air pollution in Harbin, thus leading to a signifcant increase in particle numbers (especially for PM1.0). Specifcally, coal combustion under heat supply conditions led to signifcant emissions of PM1.0 and PM2.5, especially heavy metals 2− − + and secondary atmospheric pollutants, including SO4 , NO3 , and NH4 . Natural occurrences such as dust storms in April and May, as well as straw combustion in October, also contributed to the increase in WSIs and heavy metals. The exposure risk assessment results demonstrated that Zn was the main contributor to the average daily dose through ingestion and inhalation, ADDIng and ADDinh, respectively, among the 8 heavy metals, accounting for 51.7–52.5% of the ADDIng values and 52.5% of the ADDinh values. The contribution of Zn was followed by those of Pb, Cr, Cu and Mn, while those of Ni, Cd, and Co were quite low (<2.2%). -
North and Central Asia FAO-Unesco Soil Tnap of the World 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil Map of the World
FAO-Unesco S oilmap of the 'world 1:5 000 000 Volume VII North and Central Asia FAO-Unesco Soil tnap of the world 1 : 5 000 000 Volume VIII North and Central Asia FAO - Unesco Soil map of the world Volume I Legend Volume II North America Volume III Mexico and Central America Volume IV South America Volume V Europe Volume VI Africa Volume VII South Asia Volume VIIINorth and Central Asia Volume IX Southeast Asia Volume X Australasia FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS UNITED NATIONS EDUCATIONAL, SCIENTIFIC AND CULTURAL ORGANIZATION FAO-Unesco Soilmap of the world 1: 5 000 000 Volume VIII North and Central Asia Prepared by the Food and Agriculture Organization of the United Nations Unesco-Paris 1978 The designations employed and the presentation of material in this publication do not irnply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations or of the United Nations Educa- tional, Scientific and Cultural Organization con- cerning the legal status of any country, territory, city or area or of its authorities, or concerning the delirnitation of its frontiers or boundaries. Printed by Tipolitografia F. Failli, Rome, for the Food and Agriculture Organization of the United Nations and the United Nations Educational, Scientific and Cultural Organization Published in 1978 by the United Nations Educational, Scientific and Cultural Organization Place de Fontenoy, 75700 Paris C) FAO/Unesco 1978 ISBN 92-3-101345-9 Printed in Italy PREFACE The project for a joint FAO/Unesco Soil Map of vested with the responsibility of compiling the techni- the World was undertaken following a recommenda- cal information, correlating the studies and drafting tion of the International Society of Soil Science. -
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. -
Tetrao Urogalloides) in Northeast China from 1950 to 2010 Based on Local Historical Documents
Pakistan J. Zool., vol. 48(6), pp. 1825-1830, 2016. Decline and Range Contraction of Black-Billed Capercaillie (Tetrao urogalloides) in Northeast China from 1950 to 2010 Based on Local Historical Documents Yueheng Ren, Li Yang, Rui Zhang, Jiang Lv, Mujiao Huang and Xiaofeng Luan* School of Nature Conservation, Beijing Forestry University, NO.35 Tsinghua East Road Haidian District, Beijing, P. R. China, Beijing, 100083, P. R. China, Yueheng Ren, Li Yang, Rui Zhang contributed equally. A B S T R A C T Article Information Received 21 August 2015 The black-billed capercaillie (Tetrao urogalloides) is a large capercaillie which is considered an Revised 14 March 2016 endangered species that has undergone a dramatic decline throughout the late 20th century. This Accepted 19 May 2016 species is now rare or absent in Northeast China and needs immediate protection. Effective Available online 25 September 2016 conservation and management could be hampered by insufficient understanding of the population decline and range contraction; however, any historical information, whilst being crucial, is rare. In Authors’ Contribution this paper, we present local historical documents as one problem-solving resource for large-scale YR, LY and XL conceived and designed the study. LY, YR, JL and analysis of this endangered species in order to reveal the historical population trend in Northeast MH were involved in data collection. China from 1950 to 2010. Our results show that the population was widely distributed with a large YR, LY and RZ were involved in population in Northeast China before the 1980s. Because of increasing habitat destruction in data processing. -
Mountains of Asia a Regional Inventory
International Centre for Integrated Asia Pacific Mountain Mountain Development Network Mountains of Asia A Regional Inventory Harka Gurung Copyright © 1999 International Centre for Integrated Mountain Development All rights reserved ISBN: 92 9115 936 0 Published by International Centre for Integrated Mountain Development GPO Box 3226 Kathmandu, Nepal Photo Credits Snow in Kabul - Madhukar Rana (top) Transport by mule, Solukhumbu, Nepal - Hilary Lucas (right) Taoist monastry, Sichuan, China - Author (bottom) Banaue terraces, The Philippines - Author (left) The Everest panorama - Hilary Lucas (across cover) All map legends are as per Figure 1 and as below. Mountain Range Mountain Peak River Lake Layout by Sushil Man Joshi Typesetting at ICIMOD Publications' Unit The views and interpretations in this paper are those of the author(s). They are not attributable to the International Centre for Integrated Mountain Development (ICIMOD) and do not imply the expression of any opinion concerning the legal status of any country, territory, city or area of its authorities, or concerning the delimitation of its frontiers or boundaries. Preface ountains have impressed and fascinated men by their majesty and mystery. They also constitute the frontier of human occupancy as the home of ethnic minorities. Of all the Mcontinents, it is Asia that has a profusion of stupendous mountain ranges – including their hill extensions. It would be an immense task to grasp and synthesise such a vast physiographic personality. Thus, what this monograph has attempted to produce is a mere prolegomena towards providing an overview of the regional setting along with physical, cultural, and economic aspects. The text is supplemented with regional maps and photographs produced by the author, and with additional photographs contributed by different individuals working in these regions. -
Asymmetrical Lightning Fire Season Expansion in the Boreal Forest of Northeast China
Communication Asymmetrical Lightning Fire Season Expansion in the Boreal Forest of Northeast China Cong Gao 1, Ran An 1, Wenqian Wang 1, Chunming Shi 1,* , Mingyu Wang 2,*, Kezhen Liu 3, Xiaoxu Wu 1, Guocan Wu 1 and Lifu Shu 2 1 College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China; [email protected] (C.G.); [email protected] (R.A.); [email protected] (W.W.); [email protected] (X.W.); [email protected] (G.W.) 2 Research Institute of Forest Ecology, Environment and Protection, Key Laboratory of Forest Protection of National Forestry and Grassland Administration, Chinese Academy of Forestry, Beijing 100091, China; [email protected] 3 Department of Public Security, Nanjing Forest Police College, Nanjing 210023, China; [email protected] * Correspondence: [email protected] (C.S.); fi[email protected] (M.W.) Abstract: All-season warming is assumed to advance snowmelt and delay snow accumulation; additionally, coupled with warming-induced drought stress, all-season warming could extend both the beginning and the end of the fire season. Using fire data updated for 1968–2018, we found an asymmetrical expansion of the lightning fire season in the boreal forest of Northeast China. Lightning fires have not advanced into the early fire season (May–June) but have largely extended into the snowless late fire season (July–September) since the late 1990s (mean end Julian date delayed by 51.1 days for 1998–2018 compared with 1968–1997, p < 0.001). Despite significant warming, the Julian days of snowmelt have changed only slightly, which has prohibited the fire season from advancing into early spring. -
Exploring Wintertime Regional Haze in Northeast China: Role of Coal and Biomass Burning
Atmos. Chem. Phys., 20, 5355–5372, 2020 https://doi.org/10.5194/acp-20-5355-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Exploring wintertime regional haze in northeast China: role of coal and biomass burning Jian Zhang1, Lei Liu1, Liang Xu1, Qiuhan Lin1, Hujia Zhao2, Zhibin Wang3, Song Guo4, Min Hu4, Dantong Liu1, Zongbo Shi5, Dao Huang1, and Weijun Li1 1Department of Atmospheric Sciences, School of Earth Sciences, Zhejiang University, Hangzhou, 310027, China 2Institute of Atmospheric Environment, China Meteorological Administration, Shenyang, 110016, China 3Research Center for Air Pollution and Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou, 310058, China 4State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing, 100871, China 5School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UK Correspondence: Weijun Li ([email protected]) Received: 6 November 2019 – Discussion started: 8 January 2020 Revised: 18 March 2020 – Accepted: 1 April 2020 – Published: 7 May 2020 Abstract. As one of the intense anthropogenic emission 223 µg m−3) with predominantly OM (98–133 µg m−3) and regions across the relatively high-latitude ( > 40◦ N) areas unexpectedly high KC (3.8 µg m−3). TEM also showed that on Earth, northeast China faces the serious problem of re- K-rich particles internally mixed with OM (named K-OM) gional haze during the heating period of the year. Aerosols increased from 4 %–5 % by number to 50 %–52 %. The re- in polluted haze in northeast China are poorly understood sults indicate that there were different sources of aerosol compared with the haze in other regions of China such as particles causing the Haze-I and Haze-II formation: Haze-I the North China Plain. -
Geologic Factors Affecting Seismic Monitoring in China
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geologic Factors Affecting Seismic Monitoring in China John R. Matzkoi Open-File Report 95-562 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards. Any use of trade names is for descriptive purposes only and does not imply endorsement by the U.S. Geological Survey. JReston, Virgina 1995 Geologic Factors Affecting Seismic Monitoring in China Table of Contents Introduction ...................................................... 4 Rock Environments ................................................. 4 Igneous Rocks ............................................... 4 Metamorphic and Sedimentary Rocks ................................ 5 Ground Water Occurrences and Conditions ............................ 6 Principal Tectonic Regions ............................................. 7 Active Tectonics ..................................................... 8 Quaternary Volcanism ................................................ 10 Crustal Thickness and Characteristics ..................................... 11 Seismicity ........................................................ 13 Heat Flow ........................................................ 13 Salt Deposits ...................................................... 14 Oil and Natural Gas Development ........................................ 15 Mining Regions .................................................... 16 Karst ........................................................... 17 Loess -
Study on the Spatial Differentiation of the Populations on Both Sides of the “Qinling-Huaihe Line” in China
sustainability Article Study on the Spatial Differentiation of the Populations on Both Sides of the “Qinling-Huaihe Line” in China Jie Liu 1, Qingshan Yang 1,*, Jian Liu 1 , Yu Zhang 1 , Xiaojun Jiang 2 and Yangmeina Yang 1 1 School of Geographical Science, Northeast Normal University, Changchun 130024, China; [email protected] (J.L.); [email protected] (J.L.); [email protected] (Y.Z.); [email protected] (Y.Y.) 2 Department of Resources Management, Tangshan Normal University, Tangshan 063000, China; [email protected] * Correspondence: [email protected]; Tel.: +86-043-8509-9550 Received: 31 March 2020; Accepted: 27 May 2020; Published: 3 June 2020 Abstract: The “Qinling-Huaihe Line” is the recognized geographical boundary between north and south China. In the context of a widening north–south gap, the large-scale population flow and the implementation of the regional coordinated development strategy, the north–south differentiation of the Chinese population requires further investigation. This study is based on national census data and uses quantitative methods, such as the centralization index, coefficient of variation, hot spot analysis and geodetector, as research methods. This study takes the Qinling-Huaihe Line as the dividing line and aims to extensively explore the spatial differentiation, evolutionary characteristics, and influential factors of the populations on both sides. The main conclusions are as follows: O1 From 1982 to 2010, the population share ratio on the south and north sides of the Qinling-Huaihe Line remained at 58:42, showing a distribution pattern of “South more and North less”. O2 The area within 200 km from the Qinling-Huaihe Line is a transition area with a stable distribution of the populations on both sides. -
Geography of China Shang Dynasty (1700
GEOGRAPHY OF CHINA China’s vast lands are covered by mountain ranges ZHOU and deserts. Two deserts, the Taklimakan and Gobi, prevented foreign visitors and invaders from DYNASTY(1050 - 256 BC) entering into Ancient China. The many mountain The right to rule China was determined by the ranges that cover Asia formed additional protective gods and if a dynasty no longer had the right to rule, barriers for China’s early dynasties. China’s mountains they could be conquered. The Zhou used this Mandate from the Greater Khingan Range in the northeast to of Heaven to conquer the Shang and gain control. The the Tian Shan Range in the northwest to the massive Zhou were the first dynasty to use iron. Additionally, 1500 mile Himalayas Range south of the Tibetan the Hundred Schools of Thoughts (about 770 BC - 222 Plateau all helped shape the history of Ancient China. BC), the Golden Age of Chinese philosophies, took place during their rule. In 771 BC, invaders from a neighboring kingdom forced the Zhou out of central China's Rivers China. The dynasty ruled for another 500 years, but China’s earliest dynasties began in the Huang He or the empire was smaller and less powerful. Yellow River Valley. Known as ‘China’s Sorrow’ because of its deadly and unpredictable flooding, the Yellow River flows across northern China to the Yellow Sea. QIN DYNASTY (221 - 206 BC) The river gets its name from the yellow loess (clay dust) After the Warring States period (400s - 221 BC), the that is deposited in the river as it flows across China. -
Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation • Proposal 2
Annex V. New Proposals on Three Target Feline Species of the NEASPEC Nature Conservation Strategy The following proposals have been submitted by the Russian Government in consultation with partner agencies and experts in China and Mongolia, respectively. • Proposal 1. Ensure Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation • Proposal 2. Transboundary Cooperation Between Neighbouring Protected Areas in China and Russia for Tiger Conservation in Lesser Khingan Mountains • Proposal 3. Evaluation of the Current Status of two Snow Leopard Subpopulations in Transboundary Area Between Russia and Mongolia [Proposal 1]: Transboundary Cooperation Between Neighbouring Protected Areas for Amur Leopard and Tiger Conservation The lower Tumen River area, bordered by China, DPR Korea and Russia, is the last habitat on Earth for Amur Leopard, currently estimated to number less than 100 individuals in the world, and the isolated Eastern-Manchurian population of Amur Tiger, which is now successfully recovering in North East China. Tigers and leopards come and go between China and Russia passing over the fence and sometimes reach the Korean Peninsula across the frozen river. The border is a political creation by humans, not of nature. In 2004, NEASPEC had elaborated the proposal for creation of transboundary protected area, based on existing nature reserves in Russia, China and DPRK. During last decade, the situation was really improved when the large national park “Land of leopard” (LLNP) was established in Russia in 2012, and the pilot Tiger and Leopard national park (TLNP) was launched in China. Total area of these bordering protected areas is about 1.8 million ha, which are now serves as the home for about 40 tigers and 90 leopards.