Carbon verification, which can guarantee the reliability and credibility of greenhouse gas (GHG) emission data, is the most important part of the daily operations of the carbon emission right trading system. Many international institutions, countries and regions have conducted research on and have practiced carbon verification policies and systems. Through comparative analysis of the international carbon verification policies and systems, they can provide experience for Chinese unified national carbon market to start supporting carbon verification. The paper study concludes that (1) carbon verification systems developed by international institutions focus on the scientific level of verification methods; (2) carbon verification policies and systems issued by important countries and regions draw on International Standardization Organization (ISO)14064 standards based on their national conditions and focus on the scientific level and reasonableness of verification methods; (3) major international experience includes complete verification policies and systems, strict standard verification procedures, diversified verification forms and a focus on key emission sources. Based on the differences in China’s carbon emissions characteristics caused by unbalanced regional economic development and the conditions of carbon verification in seven pilot carbon trading areas, this thesis proposes the following suggestions: pushing forward the establishment of carbon verification policies and systems by accelerating legislation on climate changes; facilitating carbon verification in a coordinated manner; regulating key GHG emission sources; establishing and improving supervision on carbon verification; and intensifying international exchanges and cooperation.
Climate variability during the Late Pleistocene is studied from the proxies in core CK-2 drilled from the Luobei Depression (91°03′E, 40°47′N), Lop Nur in the eastern Tarim Basin, Xinjiang, China. Geophysical and geochemical properties, including magnetic susceptibility, granularity, chroma, carbonate content, loss on ignition and trace elements, have been determined to reconstruct the environmental evolution of the area during 32–9 ka BP. The chronology is established by uranium–thorium disequilibrium dating techniques.Our data suggest four paleoclimate stages, indicating glacial variations between cold–humid and warm–arid environments. A period of extreme humidity occurred during 31,900–19,200 yr BP is attributed the last glacial maximum (LGM). The period was followed by a warm–arid episode during 19,200–13,500 yr BP. Then a cold–humid interval during 13,500–12,700 yr BP may correspond to another cooling phases at high latitudes of the Northern Hemisphere. The last stage from 12,700 to 9000 yr BP has a trend that the climate turned warm and arid. The Lop Nur region is characterized by particularly humid stadials and arid interstadials. The climate variability in Lop Nur was constrained by global climate change because it is correlated with Dansgaard–Oeschger and Heinrich events, which were observed at the northern high latitudes. The synchroneity of the palaeoclimatic events suggested that cold air activity at the northern high latitudes was the most important factor that influenced the climate evolution in the Lop Nur region. A probable mechanism that involves the migration of westerly winds is proposed to interpret this synchroneity. 相似文献