Fast large-scale reionization simulations     

Rajat M. Thomas  Saleem Zaroubi  Benedetta Ciardi  reas H. Pawlik  Panagiotis Labropoulos  Vibor Jeli&#;  Gianni Bernardi  Michiel A. Brentjens  A. G. de Bruyn  Geraint J. A. Harker  Leon V. E. Koopmans  Garrelt Mellema  V. N. Pandey  Joop Schaye  Sarod Yatawatta 《Monthly notices of the Royal Astronomical Society》2009,393(1):32-48

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Non-parametric foreground subtraction for 21-cm epoch of reionization experiments     

Geraint Harker  Saleem Zaroubi  Gianni Bernardi  Michiel A. Brentjens  A. G. de Bruyn  Benedetta Ciardi  Vibor Jeli&#;  Leon V. E. Koopmans  Panagiotis Labropoulos  Garrelt Mellema  ré Offringa  V. N. Pandey  Joop Schaye  Rajat M. Thomas  Sarod Yatawatta 《Monthly notices of the Royal Astronomical Society》2009,397(2):1138-1152

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新疆旅游资源新评价与开发新方略     

郭来喜 《云南地理环境研究》1993,5(2):16-22

新疆幅员广阔,深居内陆,自然复杂,人文多样,是中国旅游资源特丰区。通过组织跨部门,多学科的专家按照《中国旅游资源普查规范》(试行稿)实地考察,对新疆旅游资源的丰度、类型、功能、地域结构给出了新评价,确认它是中国旅游业发展的重要资源后备基地。从新疆地处欧亚大陆腹心,毗邻八国的特殊区位,以及世界旅游重心东移,中国旅游资源开发向内陆推进的多维多元化出发,提出了树立超前意识以市场为导向,深层次,高品位,多元化开发新疆旅游资源的新方略。即确立发展大旅游业的战略观念构建“引爆工程”、“转动效应”的特种旅游、专题旅游和常规旅游项目,完善旅游管理体制,发展以航空运输为主体的综合运输网络,强化旅游软硬件设施,建设能满足不同层次需求、富有特色功能、具有国际意义的国家级旅游地域新网络系统。  相似文献   

Heat,momentum and moisture budgets of the katabatic layer over the melting zone of the west Greenland ice sheet in summer     

Michiel R. Van Den Broeke  Peter G. Duynkerke  Edwin A. C. Henneken 《Boundary-Layer Meteorology》1994,71(4):393-413

The budgets of momentum, heat and moisture of the atmospheric boundary layer overlying the melting zone of the west Greenland ice sheet during an 8-day period in summer are calculated. To do so, the governing budget equations are derived and presented in terms of vertically averaged quantities. Moreover, stationarity is assumed in the present study. Measurements collected during the GIMEX-91 experiment are used to calculate the contribution of the different terms in the equations to the budget.During summer, a well developed katabatic wind system is present over the melting zone of the Greenland ice sheet. The budgets show that advection in the katabatic layer is small for momentum, heat and humidity, when the horizontal length scale of the integration area is sufficiently large (>50 km). This indicates that in principle one-dimensional atmospheric models can be used to study the boundary layer over the melting zone of the Greenland ice sheet. The background stratification plays a crucial role in the heat and moisture budget. Vertical divergence of longwave radiation provides one-third and the turbulent flux of sensible heat the rest of the cooling of the boundary layer. Moisture is added to the boundary layer by evaporation which is a significant term in the moisture budget. Negative buoyancy (katabatic forcing) dominates the momentum budget in the downslope direction. Coriolis forcing is important, stressing the large spatial scale of the katabatic winds on the Greenland ice sheet.  相似文献   

Identification of application-specific critical inputs for the 1991 Johnson and Ettinger vapor intrusion algorithm     

by Paul C. Johnson 《Ground Water Monitoring & Remediation》2005,25(1):63-78

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In situ mesocosms: Denitrification in the Elk Valley aquifer     

by Scott F. Korom  Allen J. Schlag  William M. Schuh  Alison Kammer Schlag 《Ground Water Monitoring & Remediation》2005,25(1):79-89

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Responsibility for Past and Future Global Warming: Uncertainties in Attributing Anthropogenic Climate Change     

Michel Den Elzen  Michiel Schaeffer 《Climatic change》2002,54(1-2):29-73

During the negotiations on the Kyoto Protocol, Brazil proposed a methodology to link the relative contribution of Annex I Parties to emission reductions with the relative contributions of Parties to the global-mean temperature increase. The proposal was not adopted during the negotiations but referred to the Subsidiary Body for Scientific and Technological Advice for consideration of its methodological aspects. In this context we analyze the impact of model uncertainties and methodological choices on the regionally attributed global-mean temperature increase. A climate assessment model has been developed to calculate changes in greenhouse gas concentrations, global-mean temperature and sea-level rise attributable to individual regions. The analysis shows the impact of the different choices in methodological aspects to be as important as the impact of model uncertainties on a region's contribution to present and future global temperature increases. Choices may be the inclusion of the anthropogenic non-CO₂ greenhouse gas emissions and/or theCO₂ emissions associated with land-use changes. When responsibility to global temperature change is attributed to all emitting Parties, the impacts of modeling uncertainties and methodological choices on contributions of individual Parties are considerable. However, if relative contributions are calculated only within the group of Annex I countries, the results are less sensitive to the uncertainty aspects considered here.  相似文献   

The pedagogy of autobiography in the history of geographic thought     

Michiel van Meeteren 《Norsk geografisk tidsskrift. Norwegian journal of geography》2019,73(4):250-255

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太湖平原碟形洼地沉积物记录的距今8000年以来植被、气候与地貌演变     

赵宝成王张华  陈中原吴国瑄 《古地理学报》2007,9(3):321-330

利用DGY孔沉积物的岩性、粒度及孢粉分析资料,探讨了太湖平原碟形洼地沉积物记录的8000年以来植被演化、气候波动,流域地貌环境的演变及其对海平面波动的响应。孢粉记录表明:本区距今8000~5000年木本植被由以落叶阔叶乔木和针叶乔木为主变为落叶阔叶乔木和常绿阔叶乔木为主,气候由温和略干转为暖热湿润;距今5000~4000年森林退缩,气候温和偏干;距今4000年左右出现低温事件;距今4000~3,000年木本植被以常绿阔叶乔木为主,气候温暖湿润;距今3000年以来木本植被主要为常绿阔叶乔木、落叶阔叶乔木和针叶乔木,气候总体温暖湿润,有波动变凉干趋势。岩性、粒度及孢粉记录综合显示本区距今8000~5000年发育潟湖相泥质粉砂,反映流域环境开放、与海连通;距今5000~4000年发育淡水沼泽,未受海水作用,反映水域缩小、流域环境封闭;距今4000~3000年水域扩大,并出现海水倒灌,反映内低外高的碟形洼地已经形成;距今3000年以来,发育湖沼平原,发生数次海水倒灌,反映碟形洼地地貌的进一步发育。  相似文献   

Protective and treatment measures against major harmful organisms in cotton-growing belt of Xinjiang     

Received date: -- Foundation item: Supported by Light of Western Regions Project  Key Project of CAS Integrated Demonstration Project for Sustainable Development of Cotton in Xinjiang with High Quality High Yield Technique LU Zhaozhi  CHEN 《地理学报(英文版)》2000,(3)

1 Harmful Organisms in Xinjiang Cotton-Growing BeltThe harmful organisms in Xinjiang cotton-growing belt are mainly diseases, insects and weeds. The diseases include Verticillium albo-atrum, cotton-root decaying disease and cotton-boll decaying disease, while the harmful insects include cotton aphids (Aphis gosspii), cotton mites, cotton boll-worms (Heliothis armigera), cotton thrips (Thrips. sp), Lygus pratersis and cutworms. Their harmful effects vary in different places but all of them …  相似文献