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61.
Environmental significance of snowpit chemistry in the typical monsoonal temperate glacier region,Baishui glacier no. 1, Mt Yulong,China 总被引:1,自引:0,他引:1
Li Zongxing He Yuanqing Pang Hongxi Wilfred H. Theakstone Zhang Ningning He Xianzhong Wang Shijing Pu Tao Du Jiankuo 《Environmental Geology》2009,58(6):1319-1328
Samples were collected from two snowpits in Baishui glacier no. 1, Mt Yulong, China, in May 2006. Snowpit chemistry was studied,
using ion tracer techniques, HYSPLIT model, factor analysis, correlation and trend analysis. It indicated that total cation
concentration is higher in 4,900-m snowpit than in 4,750-m snowpit, whereas total anion concentration is higher in 4,750-m
snowpit. Cations, especially Ca2+, dominate ionic concentrations in Baishui glacier no. 1. According to correlation analysis and factor analysis, ions can
be categorized as follows: Cl− and NO3
− as Group 1, SO4
2− as Group 2, Mg2+ and Ca2+ as Group 3, Na+ as Group 4, K+ as Group 5. Contribution made by terrestrial dust to ionic concentration accounts for 52.27, 100, 99.36, 98.91, 96.16 and
99.97% of Cl−, NO3
−, SO4
2−, K+, Mg2+ and Ca2+, respectively, in 4,900-m snowpit, and for 64.00, 100, 99.57, 98.63, 96.25 and 99.97% in 4,750-m snowpit. Local dust is the
principal source of snowpit chemical components. Pollutants brought from industrial areas of South Asia, Southeast Asia and
South China by monsoonal circulation also makes some contribution to anion concentrations, but pollution associated with human
activities makes a very slight contribution in study area. The chemical characteristics of two snowpits are different owing
to the difference of deposition mechanism and local environment in different altitudes. 相似文献
62.
利用热带大气季节内振荡(MJO)指数、向外长波辐射(OLR)资料和NCEP/NCAR全球逐日再分析资料以及中国南方地区降水资料,应用合成分析等探讨了MJO与2008年初南方雪灾的关系,进而从MJO角度研究雪灾过程成因。结果表明:雪灾过程中,MJO存在明显的东传现象,即由西太平洋向东传送至印度洋附近。伴随着MJO的向东传播,中国南方降水强度及集中区也在随之变化,MJO在一定程度上对雪灾过程有调制作用。通过对OLR的分析,表明2008年初中国南方4次异常降水(雪)过程受到了MJO两次东传的影响,第一次导致西太平洋副热带高压持续偏强,第二次导致南支槽活跃;副热带高压西侧偏南风带来的暖湿气流,以及南支槽带来的印度洋和孟加拉湾的暖湿气流不断向中国输送,为中国南方强降水过程提供了水汽条件。 相似文献
63.
Darrell R.J. Mullowney Corey J. MorrisEarl G. Dawe Katherine R. Skanes 《Marine Policy》2012,36(3):567-575
The Hawke Box trawling exclusion zone off southern Labrador is a 8610 km2 closed area implemented in 2003 to protect soft-shelled pre-recruit Snow Crab and juvenile cod from mortality imposed by shrimp trawling and other bottom-impact fisheries. This study utilizes survey, logbook, and observer data from the Snow Crab and Northern Shrimp fisheries to assess the effectiveness of the Hawke Box in protecting and possibly enhancing the Snow Crab resource off southern Labrador. The results indicate that the exclusion zone has failed to protect pre-recruit crabs largely due to a redistribution and intensification of directed Snow Crab effort inside the Box in the years following closure. This unexpected outcome resulted in a high level of fishery-induced mortality to pre-recruit crabs and masked any potential positive outcomes from the cessation of trawling. The shortcomings that contributed to the failure of this exclusion area are discussed in relation to the current state of knowledge on the effectiveness of marine protected areas in general as management tools for conserving aquatic resources. 相似文献
64.
In this paper, a new snow density estimation methodology is proposed for full-polarimetric Synthetic Aperture Radar (SAR) data. The generalized four component polarimetric decomposition with unitary transformation (G4U) based generalized volume parameter is utilized to invert snowpack dielectric constant using the Fresnel transmission coefficients. The snow density is then estimated using an empirical relationship. Six Radarsat-2 fine resolution full-polarimetric C-band datasets were acquired over Himachal Pradesh, India. The near-real time in-situ measurements were collected with the satellite pass to validate the proposed method. The mean absolute error (MAE) of the proposed method is 0.027 g cm−3 and the root mean square error (RMSE) is 0.032 g cm−3. The snow density variation within a season were also analyzed using multi-temporal Radarsat-2 data. 相似文献
65.
To model ice conditions in the eastern Gulf of Finland, a high-resolution three-dimensional hydrodynamic model is coupled with the advanced sea-ice model HELMI (Haapala et al., 2005). To test the model in extreme situations, the ice pattern in the eastern Gulf of Finland was simulated for a mild ice winter (2007–2008) and for a moderate one (2003–2004). The reference runs were performed on the assumption that the ice in the model domain is fast ice if the sea depth is less than 10 m. Using this assumption, the ice thickness averaged over the Neva Bay (the easternmost part of the Gulf of Finland) is overestimated by the model for almost the entire wintertime in the mild winter and during the ice formation and melting periods in the moderate winter, as compared with the thickness reported in ice charts. 相似文献
66.
The spatial and temporal distribution of snow cover extent (SCE) and snow water equivalent (SWE) play vital roles in the hydrology of northern watersheds. We apply remotely sensed Special Sensor Microwave Imager (SSM/I) data from 1988 to 2007 to explore the relationships between snow distribution and the hydroclimatology of the Mackenzie River Basin (MRB) of Canada and its major sub-basins. The Environment Canada (EC) algorithm is adopted to retrieve the SWE from SSM/I data. Moderate Resolution Imaging Spectroradiometer (MODIS) 8-day maximum snow cover extent products (MOD10A2) are used to estimate the different thresholds of retrieved SWE from SSM/I to classify the land cover as snow or no snow for various sub-basins in the MRB. The sub-basins have varying topography and hence different thresholds that range from 10 mm to 30 mm SWE. The accuracy of snow cover mapping based on the combination of several thresholds for the different sub-basins reaches ≈ 90%. The northern basins are found to have stronger linear relationships between the date on which snow cover fraction (SCF) reaches 50% or when SWE reaches 50% and mean air temperatures, than the southern basins. Correlation coefficients between SCF, SWE, and hydroclimatological variables show the new SCF products from SSM/I perform better than SWE from SSM/I to analyze the relationships with the regional hydroclimatology. Statistical models relating SCF and SWE to runoff indicate that the SCF and SWE from EC algorithms are able to predict the discharge in the early snow ablation seasons in northern watersheds. 相似文献
67.
68.
69.
Snow chemistry on the glaciers of alpine regions is a good indicator of atmospheric environmental change.We examine snow chemistry in three snowpits at different altitudes on the Haxilegen Glacier No.51,in the Kuitun River source,Tian Shan,China,during July-September 2004 to 2007.We use correlation analysis,factor analysis and sea-salt tracing methods to examine the characteristics and sources of major ions and mineral dust particles in the snow.Results show that mineral dust particles and major ions in the snow pits vary seasonally.During the Asian dust period in springtime,the concentration of mineral dust particles and major ions deposited in snow is high,while the concentration is relatively low during the non-dust period of summer and autumn.This may be caused by dust storm activity in central Asia.The order of major ionic concentrations in the snow packs was determined to be Ca2+ > SO42-> NH4+ > NO3-> Cl-> Na+ > Mg2+ > K+.Ca2+ was the dominant cation;SO42- was the dominant anion.We find,with the exception of NO3-,that the variabilities of ionic concentrations are highly correlated.Results show that the glacier region was significantly affected by dust activity and anthropogenic source.The major ions,especially Na+,originate from dust sources of central Asia and from the Ocean,transported by the westerly winds. 相似文献
70.
巴丹吉林沙漠周边地区近50 a来气候变化特征 总被引:7,自引:4,他引:3
利用巴丹吉林沙漠周边9个气象站的1960—2009年逐月平均气温、平均最高气温、平均最低气温、降水量、平均相对湿度和日照时数及1960—2008年逐月平均风速的观测资料,运用线性回归、滑动平均和Mann-Kendall突变检验分析了该区近50 a来气候变化特征。结果表明,近50 a来,巴丹吉林沙漠周边地区年平均气温以0.40 ℃/10a的速率显著升高;四季平均气温的升高亦很显著,以冬季的升温速率最大;年、季节平均最高气温和平均最低气温均呈显著升高趋势;年、季平均日较差则显著减小,且以最低气温的升温速率大于最高气温的升温速率为特点。年降水量以0.87 mm/10a的速率呈不显著增加趋势;各季节降水量变化略有差异且均不显著,春季降水量略有减少,夏、秋和冬季略有增加。湿润指数的变化不明显,总体来看,年和冬季湿润指数略有增大,春、夏和秋季湿润指数略有减小。年日照时数以34.8 h/10a的速率显著增加,各季节日照时数亦均有增加趋势,其中春季增加最为明显。年平均风速以-0.092 m·s-1·(10a)-1的速率呈显著减小趋势;各季节平均风速均显著减小,以冬季的减小速率最大。 相似文献