青藏高原希夏邦马冰芯中阴阳离子的研究

本文对希夏邦马浅冰芯的资料进行了分析,发同离子含量变化显示强烈的周期性变化,反映了季节变化的特征。离子浓度高低变化将指示气候的冷暖变化。并与降水量变化有着反相关关系,与δ＾１８Ｏ存在着对应关系,但δ＾１８Ｏ对气候变化的反映没有各咱郭反映灵敏。     

EFFECT OF SIMULATED CLIMATE CHANGE ON SNOWMELT RUNOFF MODELING IN SELECTED BASINS1

ABSTRACT: The projected increase in the concentration of CO₂ and other greenhouse gases in the atmosphere is likely to result in a global temperature increase. This paper reports on the probable effects of a temperature increase and changes in transpiration on basin discharge in two different mountain snowmelt regions of the western United States. The hydrological effects of the climate changes are modeled with a relatively simple conceptual, semi-distributed snowmelt runoff model. Based on the model results, it may be concluded that increased air temperatures will result in a shift of snowmelt runoff to earlier in the snowmelt season. Furthermore, it is shown that it is very important to include the expected change in climate-related basin conditions resulting from the modeled temperature increase in the runoff simulation. The effect of adapting the model parameters to reflect the changed basin conditions resulted in a further shift of streamflow to April and an even more significant decrease of snowmelt runoff in June and July. If the air temperatures increase by approximately 5°C and precipitation and accumulated snow amounts remain about the same, runoff in April and May, averaged for the two basins, is expected to increase by 185 percent and 26 percent, respectively. The runoff in June and July will decrease by about 60 percent each month. Overall, the total seasonal runoff decreases by about 6 percent. If increased CO₂ concentrations further change basin conditions by reducing transpiration by the maximum amounts reported in the literature, then, combined with the 5°C temperature increase, the April, May, June, and July changes would average +230 percent, +40 percent, ?55 percent, and ?45 percent, respectively. The total seasonal runoff change would be +11 percent.     

APPLICATION OF THE SNOWMELT RUNOFF MODEL USING MULTIPLE-PARAMETER LANDSCAPE ZONES ON THE TOWANDA CREEK BASIN,PENNSYLVANIA1

ABSTRACT: The Snowmelt Runoff Model (SRM) is designed to compute daily stream discharge using satellite snow cover data for a basin divided into elevation zones. For the Towanda Creek basin, a Pennsylvania watershed with relatively little relief, analysis of snow cover images revealed that both elevation and land use affected snow accumulation and melt on the landscape. The distribution of slope and aspect on the watershed was also considered; however, these landscape features were not well correlated with the available snow cover data. SRM streamflow predictions for 1990, 1993 and 1994 snowmelt seasons for the Towanda Creek basin using a combination of elevation and land use zones yielded more precise streamflow estimates than the use of standard elevation zones alone. The use of multiple-parameter zones worked best in non-rain-on-snow conditions such as in 1990 and 1994 seasons where melt was primarily driven by differences in solar radiation. For seasons with major rain-on-snow events such as 1993, only modest improvements were shown since melt was dominated by rainfall energy inputs, condensation and sensible heat convection. Availability of GIS coverages containing satellite snow cover data and other landscape attributes should permit similar reformulation of multiple-parameter watershed zones and improved SRM streamflow predictions on other basins.     

SNOW AND ICE ALBEDO MEASURED WITH TWO TYPES OF PYRANOMETERS1

ABSTRACT: In order to obtain total short-wave albedos of snow and ice, both incident and reflected solar radiation were measured over a frozen lake surface using two different types of radiation measurement devices: a Kipp and Zonen thermopile pyranometer with a spectral sensitivity of 300 to 2800 nm and a LI-COR photovoltaic pyranometer with a spectral sensitivity of 400 to 1100 am. The spectral response of the LI-COR pyranometers limits its use as a short-wave radiation measurement device. Therefore, two equations were developed to adjust both the daily incident radiation data and the daily reflected radiation data measured by the LI-COR instrument to total short-wave radiation values, i.e., to the waveband of 300 to 2800 nm (visible to near-infrared spectrum). The LI-COR data were then adjusted, and a total short-wave adjusted albedo was calculated with a modeling efficiency of 0.97.     

冰情预报的投影寻踪回归模型

将投影寻踪回归模型应用于黑龙江上游江段开河日期的预报,并与GA-BP模型预报的结果进行了对比分析.结果表明,投影寻踪回归模型预报的精度及稳定性较高,其性能优于常用的GA-BP模型.预报采用理论分析与多元逐步回归分析相结合的方法筛选预报因子,既可确保不遗漏基本影响因子,又能剔除对目标值影响不显著的因子,用于确定冰情预报的预报因子较为适宜.     

悬浮结晶法冷冻处理喹乙醇生产废液

采用悬浮结晶法处理喹乙醇生产废液,考察了成冰率(冰晶融化后的体积占原水总体积的百分比)对废液COD、氨氮、TN和电导率去除效果的影响。在一级冷冻成冰率45%的条件下,经过三级冷冻处理后,三级出水的COD、氨氮、TN和电导率的去除率分别为99.4%、98.7%、98.5%和98.2%,一级浓缩液的COD、氨氮和TN的浓缩比分别为1.6、1.5和1.5;在一级冷冻成冰率80%的条件下,每一级出水的各项指标的去除率均有所下降,三级出水的COD、氨氮、TN和电导率的去除率分别为98.6%、98.3%、97.1%和95.9%,但一级浓缩液的浓缩比明显提高,COD、氨氮和TN的浓缩比分别为2.7、2.2和2.4。成冰率为80%时一级浓缩液的热值为7 449 J/g,在焚烧过程中可以依靠自身热量维持燃烧,不需要添加辅助燃料,减少焚烧处理的成本。     

冰晶中双氧水的UV光解

本文采用253.7 nm的紫外灯光解冰晶中的双氧水,研究其光解率随光照时间和温度的变化.以及Cl~-,SO_4~(2-)和CO_3~(2-)对其降解的影响,结果表明,相同条件下三种离子对其影响大小依次为:Cl~->SO_4~(2-)>CO_3~(2-).对比冰晶和水溶液中双氧水的光解,冰晶中双氧水的光解速率低于水溶液中双氧水的光解速率.紫外-可见光谱(UV-vis)分析其光解产物,没有发现新的物质生成.由此可以认为,冰晶中双氧水主要在冰晶笼子中进行反应,少部分在类似液体层(QLL)中降解.     

基于EOS/MODIS卫星遥感数据的渤海海冰变化趋势及特征应用研究

根据卫星遥感数据的分辨率、采集频次、获取方式等特点,将MODIS卫星遥感数据应用到渤海海冰遥感监测中。通过海冰在可见光和红外光波段的光谱存在特定差异的特性,对海冰发生面积进行提取。同时对渤海海冰进行了遥感监测,并完整地监测到海冰从发生到极盛再到消退的全过程。同时,在海冰发生最为严重的时段,对辽东湾海域进行了密集监测。研究结果表明,MODIS卫星遥感数据在海冰监测中有着及时、准确的优势。     

利用AVHRR和MODIS数据测算海冰资源量——以渤海海冰资源测算为例

论文探讨了利用遥感数据测算海冰资源量的方法,提出了基于GIS技术和光谱特征的海冰信息分层提取法,并测算出2001-01-15的渤海海冰资源储量和可开采量分别为8.19×109m3和4×1010m3,表明渤海海冰作为淡水资源,其数量是相当可观的。论文认为,利用可见光、近红外和远红外波段对海冰资源量测算效果明显;MODIS数据在海冰资源量测算方面优于AVHRR数据。     

冰雪中持久性有机污染物（POPs）的研究现状

冰雪是地球生态系统中重要的环境组分,它们不仅直接影响着全球的水循环,而且也直接影响着一些物质在不同纬度和海拔上的分布。随着气候的变化,在中低纬度使用和排放的POPs能够挥发到大气中,并伴随着大气的运动向高纬度高海拔地区迁移,这对生态环境造成了极大的威胁。本文主要介绍了持久性有机污染物的危害、历史排放数据,并详细阐述了国内外研究人员对冰雪中POPs的研究现状。