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61.
气候变暖对新疆乌昌地区棉花种植区划的影响 总被引:6,自引:0,他引:6
在对新疆乌昌地区1961-2010年≥10℃积温、最热月(7月)平均气温和无霜期等热量要素时空变化进行分析的基础上,结合北疆棉区区划指标,完成了2004年前、后乌昌地区棉花种植气候区划。并对未来年平均气温升高1~4℃时,棉花种植气候区划的可能变化进行了预估。结果表明:乌昌地区热量资源在空间分布上表现为“平原多,山区少”的格局。1961-2010年≥l0℃积温、最热月平均气温和无霜期分别以每10年52.3℃• d、0.1℃和3.3 d的速率增多(升高、延长),并分别于1995年、2004年和1987年发生了突变。受其影响,2004年后乌昌地区宜棉区较之前明显扩大,次宜棉区、风险棉区和不宜棉区有不同程度的缩小。未来气候变暖将对乌昌地区棉花种植气候区划产生较大影响,年平均气温每升高1℃,宜棉区面积将扩大6600 km2,次宜棉区和不宜棉区分别缩小2100 km2和4700 km2,风险棉区面积变化不大。 相似文献
62.
Geological and geochemical characteristics of Middle Jurassic granites in Bengbu uplift, Southeast of North China craton 总被引:1,自引:0,他引:1
<正>1 Introduction The early formation and evolution of the North China craton has been widely concerned by scientists.The Bengbu uplift belt is located in the southeast of the craton,theresearch degree of the belt is relatively low and received increasing attention from many scholars in recent years.Through the author's practical work and combined with 相似文献
63.
The history of water salinity in the Pearl River estuary,China, during the Late Quaternary 总被引:1,自引:0,他引:1
Yongqiang Zong Fengling Yu Guangqing Huang Jeremy M. Lloyd Wyss W.‐S. Yim 《地球表面变化过程与地形》2010,35(10):1221-1233
This research reconstructed the Late Quaternary salinity history of the Pearl River estuary, China, from diatom records of four sedimentary cores. The reconstruction was produced through the application of a diatom–salinity transfer function developed based on 77 modern surface sediment samples collected across the estuary from shallow marine environment to deltaic distributaries. The statistical analysis indicates that the majority of sediment samples from the cores has good modern analogues, thus the reconstructions are reliable. The reconstructed salinity history shows the older estuarine sequence formed during the last interglacial was deposited under similar salinity conditions to the younger estuarine sequence, which was formed during the present interglacial. Further analysis into the younger estuarine sequence reveals the interplays between sea level, monsoon‐driven freshwater discharge, and deltaic shoreline movement, key factors that have influenced water salinity in the estuary. In particular, a core from the delta plain shows the effects of sea‐level change and deltaic progradation, while cores from the mouth region of the estuary reveal changes of monsoon‐driven freshwater discharge. This study demonstrates the advantages of quantitative salinity reconstructions to improve the quality of reconstruction and allow direct comparison with other quantitative records and the instrumentally observed values of salinity. Copyright © 2010 John Wiley & Sons, Ltd. 相似文献
64.
梅州市地处粤东北,由于历史、地理环境、发展基础等多方面原因,经济发展比较缓慢,属于经济欠发达山区。梅州市是我国历史文化名城、全国优秀旅游城市、世界客都、广东省重要的生态屏障,比较优势和后发优势明显。梅州市应在科学发展观的指导下,把自身优势转化为支撑经济发展的强劲动力和科学发展的实际成果,大力发展绿色经济,构建符合节能减排时代主旋律的新型产业体系,实现经济的快速发展。通过比较分析,揭示了梅州市经济发展存在的主要问题,阐述了梅州市的比较优势,探索梅州市实现经济跨越式发展路径和战略选择。 相似文献
65.
The South China Sea (SCS) is significantly influenced by El Niño and the Southern Oscillation (ENSO) through ENSO-driven atmospheric and oceanic changes. We analyzed measurements made from 1960 to 2004 to investigate the interannual variability of the latent and sensible heat fluxes over the SCS. Both the interannual variations of latent and sensible heat fluxes are closely related to ENSO events. The low-pass mean heat flux anomalies vary in a coherent manner with the low-pass mean Southern Oscillation Index (SOI). Time lags between the heat flux anomalies and the SST anomalies were also studied. We found that latent heat flux anomalies have a minimum value around January of the year following El Niño events. During and after the mature phase of El Niño, a change of atmospheric circulation alters the local SCS near-surface humidity and the monsoon winds. During the mature phase of El Niño, the wind speed decreases over the entire sea, and the air-sea specific humidity difference anomalies decreases in the northern SCS and increases in the southern SCS. Thus, a combined effect of wind speed anomalies and air-sea specific humidity difference anomalies results in the latent heat flux anomalies attaining minimum levels around January of the year following an El Niño year. 相似文献
66.
Wenjiao Shi Yunfeng Hu Xiaoli Shi Zong Wang Huimin Yan Ziwei Xu Bo Ren Wenhui Kuang Xinliang Xu Weiming Cheng Yan Chen Dongbo Wu 《地理学报(英文版)》2016,26(12):1675-1688
Strategic transformation of regionalization for agricultural comprehensive development (ACD) was presented by the Ministry of Finance of the People’s Republic of China (MOF) in 2014. The regionalization is the premise and basis of the sustainable development and improved competitiveness for agriculture. Based on the environmental resources related to agriculture, such as cropland, climate, water resources, terrain, geomorphology, patterns of the ACD projects, distribution of ecological planning, etc., we devised 13 indices using the geographic comprehensive regionalization method. The indices took into account a combination of dynamic and static, qualitative and quantitative, as well as agricultural and ecological factors. The strategic transformation of regionalization for the ACD in Ningxia Hui Autonomous Region of China was performed; seven types were included: prioritized regions, prioritized and restricted regions, protected regions, protected and restricted regions, restricted and prioritized regions, restricted and protected regions, and restricted regions. A further 24 subtypes were used based on locations and ecological zones. The regionalization results showed that prioritized regions were mainly in northern Ningxia, the most suitable area for agriculture. The protected and restricted regions were in central and southern Ningxia. In the central part, drought was the limiting factor for agriculture, and water conservation projects there should be supported. The ecological environment is fragile in southern Ningxia, so there is a need for ecologically sound agriculture to be developed in this region. Such regionalization could achieve two goals, namely agricultural conservation and eco-environmental protection. It was performed following the requirement for scientific regionalization to include three types of regions (prioritized regions, protected regions, and restricted regions), and was applied at the township scale in a provincial or autonomous region for the first time. The results provide both guidance for the strategic transformation of the ACD in Ningxia, and a reference for similar work in other provinces. 相似文献
67.
Landslides generate enormous volumes of sediment in mountainous watersheds; however, quantifying the downstream transport of landslide‐derived sediment remains a challenge. Landslide erosion and sediment delivery to the Shihmen Reservoir watershed in Taiwan was estimated using empirical landslide frequency–area and volume–area relationships, empirical landslide runout models, and the Hydrological Simulation Program‐ FORTRAN (HSPF). Landslide erosion rates ranged from 0.4 mm yr‐1 to 2.2 mm yr‐1 during the period 1986–2003, but increased to 7.9 mm yr‐1 following Typhoon Aere in 2004. The percentage of landslide sediment delivered to streams decreased from 78% during the period 1986–1997 to 55% in 2004. Although the delivery ratio was lower, the volume of landslide sediment delivered to streams was 2.81 × 106 Mg yr‐1 in 1986–1997 and 8.60 × 106 Mg yr‐1 in 2004. Model simulations indicate that only a small proportion of the landslide material was delivered downstream. An average of 13% of the landslide material delivered to rivers was moved downstream during the period 1986–1997. In 2004, the period including Typhoon Aere, the annual fluvial sediment yield accounted for approximately 23% of the landslide material delivered to streams. In general, the transfer of sediment in the fluvial system in the Shihmen Reservoir watershed is dominantly transport limited. The imbalance between sediment supply and transport capacity has resulted in a considerable quantity of landslide material remaining in the upper‐stream regions of the watershed. Copyright © 2012 John Wiley & Sons, Ltd. 相似文献
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70.
柴达木盆地干柴沟地区油气成藏条件及其勘探意义 总被引:5,自引:0,他引:5
干柴沟地区烃源岩发育良好 ,具有较为有利的油气储、盖层 ,特别是在其东南部和南北向古构造带中油气勘探前景良好 ,但构造圈闭和有利的岩相带的相匹配 ,才是形成干柴沟地区油气藏的关键 相似文献