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81.
Prior research on retail shrinkage has taken a largely individual‐level approach to theorizing about why it occurs, showing that older employees are less prone to theft and more vigilant in preventing customer shoplifting than younger personnel. However, given the influence of organizational contexts on organizational behavior, theorizing about shrinkage may be enhanced by the consideration of business‐unit level contextual variables. The present study addressed this concern by examining the relationship between store‐level age composition, whistle‐blowing (WB) climate, and shrinkage in 726 retail stores. Results indicated that the negative mean age–shrinkage relationship was stronger when there was less age diversity or a climate more supportive of WB. Moreover, the negative WB climate–shrinkage linkage was stronger when the mean age was higher. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献
82.
83.
Viktor Baranov Jonas Jourdan Francesca Pilotto Rüdiger Wagner Peter Haase 《Conservation biology》2020,34(5):1241-1251
The ongoing biodiversity crisis becomes evident in the widely observed decline in abundance and diversity of species, profound changes in community structure, and shifts in species’ phenology. Insects are among the most affected groups, with documented decreases in abundance up to 76% in the last 25–30 years in some terrestrial ecosystems. Identifying the underlying drivers is a major obstacle as most ecosystems are affected by multiple stressors simultaneously and in situ measurements of environmental variables are often missing. In our study, we investigated a headwater stream belonging to the most common stream type in Germany located in a nature reserve with no major anthropogenic impacts except climate change. We used the most comprehensive quantitative long-term data set on aquatic insects available, which includes weekly measurements of species-level insect abundance, daily water temperature and stream discharge as well as measurements of additional physicochemical variables for a 42-year period (1969–2010). Overall, water temperature increased by 1.88 °C and discharge patterns changed significantly. These changes were accompanied by an 81.6% decline in insect abundance, but an increase in richness (+8.5%), Shannon diversity (+22.7%), evenness (+22.4%), and interannual turnover (+34%). Moreover, the community's trophic structure and phenology changed: the duration of emergence increased by 15.2 days, whereas the peak of emergence moved 13.4 days earlier. Additionally, we observed short-term fluctuations (<5 years) in almost all metrics as well as complex and nonlinear responses of the community toward climate change that would have been missed by simply using snapshot data or shorter time series. Our results indicate that climate change has already altered biotic communities severely even in protected areas, where no other interacting stressors (pollution, habitat fragmentation, etc.) are present. This is a striking example of the scientific value of comprehensive long-term data in capturing the complex responses of communities toward climate change. 相似文献
84.
江苏省植被NPP时空特征及气候因素的影响 总被引:3,自引:0,他引:3
利用2000—2006年的EOS/MODIS卫星遥感资料,对江苏省植被净初级生产力(NPP)时空特征及气候变化对其影响进行分析。在ArcGIS软件中,建立线性回归方程获得NPP的变化斜率,分析7 a间各像元NPP的空间变化趋势。计算各像元的NPP数值与气候要素的线性相关系数,为定量阐述气候变化对植被生长的影响提供依据。结果表明,江苏省植被NPP 7 a平均值为506.6 g.m-2.a-1(以C计),比全国同期NPP数值高出约40%。NPP表现出明显的年际变化,2004年植被年均NPP最大为530.6 g.m-2.a-1(以C计),2000年最小,为481.1 g.m-2.a-1(以C计)。空间分布上NPP表现为东南高于西北,沿海高于内陆。2000—2006年江苏省有76%的区域植被NPP表现为显著增加,仅江苏南部少数区域表现出减少的趋势。除苏南少数区域外,气候因素控制着NPP的时空变化规律。其中气温的升高和太阳辐射的增加促进NPP提高,而降水量的增加引起NPP的降低。 相似文献
85.
2000—2007年珠峰自然保护区植被时空变化与驱动因子 总被引:1,自引:0,他引:1
采用遥感与GIS相结合的方法研究了珠峰自然保护区2000—2007年之间的植被时空变化过程和驱动机制问题。通过一元线性回归斜率计算获取了基于EVI数据的珠峰自然保护区植被变化趋势,以及表现2000—2007年植被变化的矢量图层。利用GIS时间动画技术,建立了7个时间点内不同间隔的植被时空演化过程快照,并结合ArcEngine构建了植被变化监测的时序分析流程,提取和分析了植被变化过程的时空特征。依据年平均温和年降水量观测记录进行了植被变化的气候因子分析,依据道路、河流缓冲区的居民点密度与植被退化面积比例的相关性,分析了人类活动影响,并讨论了不同植被退化区域在多重因素作用下的变化驱动因子。拟合了主要社会经济发展指标与植被变化的相关性,从统计数据方面讨论了珠峰自然保护区社会经济发展对植被变化的影响作用。结果表明:珠峰自然保护区植被变化的总体趋势以稳定为主,但植被退化趋势超过了变好趋势。同时,核心区植被变好趋势明显,实验区植被退化趋势严重。保护区南坡植被受气候变化干扰小,保持了大部分变好趋势;北坡由于降水减少造成湿地植被退化,对草地的长势带来消极作用。人类活动与植被状态变化有密切关系,在沟谷地带的破坏作用明显。并且,植被退化趋势与农业耕地面积扩大以及放牧影响关联紧密,而牲畜饲养与林业发展都未对保护区植被变化造成明显影响。 相似文献
86.
基于辽宁省56个气象站的气象资料,利用Kira的温暖指数(WI)、寒冷指数(CI)和徐文铎的湿度指数(HI)分析辽宁省近40年(1967-2006年)气候-植被指标的时空变异。结果表明,就辽宁省区域平均值而言,WI指数呈升高趋势,每10年增加幅度为2.47℃·月,CI指数呈下降趋势,每10年下降幅度为2.31℃·月,HI总体呈下降趋势,波动较WI和CI明显,从气候—植被指数变化趋势看,对红松Pinus koraiensis Sieboldet Zuccarini、长白落叶松Larixolgensis等不利,而对油松Pinu stabulaeformis Carr、栓皮栎Quercus vari abilis Blume等树种有利。空间变化特征表现为,温暖指数界限呈向西北移动的趋势,表明暖温带落叶阔叶疏林带的适宜面积增加,而温带针阔叶混交林带的适宜面积减小;HI指数减小并且向东移,表明随着指数带的北移和东移缩小限制了原有针叶树种的生长,而对栎树Phytophthora ramorum等阔叶树种有利。 相似文献
87.
Abstract: To anticipate the rapidly changing world resulting from global climate change, the projections of climate models must be incorporated into conservation. This requires that the scales of conservation be aligned with the scales of climate-change projections. We considered how conservation has incorporated spatial scale into protecting biodiversity, how the projections of climate-change models vary with scale, and how the two do or do not align. Conservation planners use information about past and current ecological conditions at multiple scales to identify conservation targets and threats and guide conservation actions. Projections of climate change are also made at multiple scales, from global and regional circulation models to projections downscaled to local scales. These downscaled projections carry with them the uncertainties associated with the broad-scale models from which they are derived; thus, their high resolution may be more apparent than real. Conservation at regional or global scales is about establishing priorities and influencing policy. At these scales, the coarseness and uncertainties of global and regional climate models may be less important than what they reveal about possible futures. At the ecoregional scale, the uncertainties associated with downscaling climate models become more critical because the distributions of conservation targets on which plans are founded may shift under future climates. At a local scale, variations in topography and land cover influence local climate, often overriding the projections of broad-scale climate models and increasing uncertainty. Despite the uncertainties, ecologists and conservationists must work with climate-change modelers to focus on the most likely projections. The future will be different from the past and full of surprises; judicious use of model projections at appropriate scales may help us prepare. 相似文献
88.
Abstract: To be successful, conservation practitioners and resource managers must fully integrate the effects of climate change into all planning projects. Some conservation practitioners are beginning to develop, test, and implement new approaches that are designed to deal with climate change. We devised four basic tenets that are essential in climate-change adaptation for conservation: protect adequate and appropriate space, reduce nonclimate stresses, use adaptive management to implement and test climate-change adaptation strategies, and work to reduce the rate and extent of climate change to reduce overall risk. To illustrate how this approach applies in the real world, we explored case studies of coral reefs in the Florida Keys; mangrove forests in Fiji, Tanzania, and Cameroon; sea-level rise and sea turtles in the Caribbean; tigers in the Sundarbans of India; and national planning in Madagascar. Through implementation of these tenets conservation efforts in each of these regions can be made more robust in the face of climate change. Although these approaches require reconsidering some traditional approaches to conservation, this new paradigm is technologically, economically, and intellectually feasible. 相似文献
89.
Abstract: Given their physiological requirements, limited dispersal abilities, and hydrologically sensitive habitats, amphibians are likely to be highly sensitive to future climatic changes. We used three approaches to map areas in the western hemisphere where amphibians are particularly likely to be affected by climate change. First, we used bioclimatic models to project potential climate‐driven shifts in the distribution of 413 amphibian species based on 20 climate simulations for 2071–2100. We summarized these projections to produce estimates of species turnover. Second, we mapped the distribution of 1099 species with restricted geographic ranges. Finally, using the 20 future climate‐change simulations, we mapped areas that were consistently projected to receive less seasonal precipitation in the coming century and thus were likely to have altered microclimates and local hydrologies. Species turnover was projected to be highest in the Andes Mountains and parts of Central America and Mexico, where, on average, turnover rates exceeded 60% under the lower of two emissions scenarios. Many of the restricted‐range species not included in our range‐shift analyses were concentrated in parts of the Andes and Central America and in Brazil's Atlantic Forest. Much of Central America, southwestern North America, and parts of South America were consistently projected to experience decreased precipitation by the end of the century. Combining the results of the three analyses highlighted several areas in which amphibians are likely to be significantly affected by climate change for multiple reasons. Portions of southern Central America were simultaneously projected to experience high species turnover, have many additional restricted‐range species, and were consistently projected to receive less precipitation. Together, our three analyses form one potential assessment of the geographic vulnerability of amphibians to climate change and as such provide broad‐scale guidance for directing conservation efforts. 相似文献
90.
热带增宽及其对中国东部亚热带森林植被的影响 总被引:2,自引:0,他引:2
全球气候变暖已是不争的事实,现今气候变暖的趋势已由每百年(1901--2000)增加0.6℃的记录升高为0.74℃(1906—2005)。其中高纬度地区增温特别显著,成为世界关注的热点。与之对比,热带地区的气候变化以及热带森林对它的反应报道甚少。事实上,自1970s中期以来,热带温度是每lO年升高0.26oC;同时气候模型预测到本世纪末热带地区温度将上升2.1-4.5℃。这些预测是有根据的,但究竟不是直接的证据。因此,本文综合了许多专家对热带地球物理学和大气层特性的多年观测、分析和研究的成果,其结论认为:至少自1979年以来许多热带大气层固有的特征发生变化并向地球极地推进和位移,这些根据是:(1)热带高空的哈德利环流增强并向极地扩展;(21位于热带边缘的亚热带射流向极地移动;(3)热带亚热带对流层顶高度和位置的变化;(4)热带高空平流层臭氧柱总量浓度的变化。据上述特征的变化证明数十年来热带向极地增宽纬度2°~5°(~8°),一般确认为2.5°。由于热带增宽的驱动,广东50年的气温记录表明气候持续变暖,按增暖趋势推算,预估到2020年,现在的雷州半岛南部可能变成中热带;广东东南沿海将由目前的南亚热带变为北热带(占全省面积约1/3);其余大部分地区为南亚热带;中亚热带基本上将退出广东(仅剩下东北角一偶)。此预测意味着南岭地区将成为南亚热带的边缘地。 相似文献