基于植被光合有效辐射资料研究中国地区植被大气反馈作用          下载免费PDF全文

唐健  汤剑平 《地球物理学报》2012,55(6):1804-1816

本文采用中国地区基于卫星观测的植被光合有效辐射资料(FPAR)和月平均气候数据(1982-2000年)来分析中国区域陆面植被与气温、降水的反馈作用.通过计算和分析超前滞后相关系数和反馈系数发现:春、夏季FPAR超前气温一个月相关系数在全国大部分地区为负值,反映出植被生长旺盛,可以降低局地气温.春、秋两季气温与FPAR的同期相关系数较大.夏季降水超前FPAR一个月的正相关性反映出夏季降水对于植被生长存在促进作用.在中国长江流域以南区域,植被对于气温的反馈系数为一致正值,可达0.5 ℃(0.1FPAR)^-1;在30°N以北区域显示出一致的负反馈,可达-0.42 ℃(0.1FPAR)^-1.FPAR对降水全年反馈系数全国区域平均可达-2.12 cm month^-1(0.1FPAR)^-1.不同植被类型、不同季节的植被反馈效应也存在差异.植被反馈系数可以用来验证动态植被模式计算的植被大气反馈作用.  相似文献   

论土地利用转型与土地资源管理   总被引：40，自引：11，他引：29  

龙花楼 《地理研究》2015,34(9):1607-1618

自21世纪初土地利用转型这一研究方向引入中国后,土地利用转型已成为当今学术界和国家行政部门十分关注的重要课题。在拓展深化土地利用转型的概念内涵,阐述土地利用转型的理论模式基础上,探讨了土地利用转型与土地资源管理二者之间的互馈机制,进而分析了土地利用转型与土地资源管理二者之间的相互影响。研究指出：决策部门应根据土地利用形态的变化适时调整土地资源管理政策措施,充分考虑目标区域所处的土地利用转型阶段,以增强土地资源管理决策的科学性。在探讨未来土地利用转型与土地资源管理研究方向基础上,强调土地利用隐性形态及其变化应当成为今后土地利用转型与土地资源管理研究关注的焦点,通过管控土地利用隐性形态的变化来创新土地资源管理政策法规及制度,提升土地资源管理水平。  相似文献   

Model‐based multi‐metric control of uniaxial shake tables          下载免费PDF全文

Brian M. Phillips  Nicholas E. Wierschem  B. F. Spencer Jr. 《地震工程与结构动力学》2014,43(5):681-699

Shake tables provide a direct means by which to evaluate structural performance under earthquake excitation. Because the entire structure is mounted on the base plate and subjected to the ground motion in real time, dynamic effects and rate‐dependent behavior can be accurately represented. Shake table control is not straightforward as the desired signal is an acceleration record, while most actuators operate in displacement feedback for stability. At the same time, the payload is typically large relative to the capacity of the actuator, leading to pronounced control‐structure interaction. Through this interaction, the dynamics of the specimen influence the dynamics of the shake table, which can be problematic when specimens change behavior because of damage or other nonlinearities. Moreover, shake tables are themselves inherently nonlinear, making it difficult to accurately recreate a desired acceleration record over a broad range of amplitudes and frequencies. A model‐based multi‐metric shake table control strategy is proposed to improve tracking of the desired acceleration of a uniaxial shake table, remaining robust to nonlinearities including changes in specimen condition. The proposed strategy is verified for the shake table testing of both linear and nonlinear structures. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   

盾构施工地表沉降自动化监测及数据移动发布系统     

谢雄耀  李军  王强 《岩土力学》2016,37(Z2):788-794

地表沉降监测是盾构信息化施工的重要组成部分,对优化盾构施工参数,保证施工安全具有十分重要的意义。为了及时共享和反馈监测成果,提高监测信息管理与数据分析的效率,采用Microsoft Visual Studio .Net编程技术和MySQL数据库开发了沉降自动化监测及数据移动发布系统,实现了24 h监测数据的自动化采集、分析和移动端推送,并将该系统应用于南宁轨道交通1号线盾构隧道下穿南宁火车站铁路股道及站房工程,获得盾构推进过程中的地表沉降及火车轨道沉降的变化规律。通过监测数据和分析成果的及时反馈,优化了盾构机施工参数,有效保证了盾构掘进和周边环境的安全。  相似文献   

Model‐based evaluation of impact of soil redistribution on soil organic carbon stocks in a temperate hedgerow landscape          下载免费PDF全文

Marine Lacoste  Valérie Viaud  Didier Michot  Christian Walter 《地球表面变化过程与地形》2016,41(11):1536-1549

Agroforestry systems are promoted for providing a number of ecosystem services and environmental benefits, including soil protection and carbon sequestration. This study proposes a modelling approach to quantify the impact of soil redistribution on soil organic carbon (SOC) storage in a temperate hedgerow landscape. Evolution of SOC stocks at the landscape scale was examined by simulating vertical and horizontal SOC transfers in the 0–105 cm soil layer due to soil redistribution by tillage and water processes. A spatially explicit SOC dynamics model (adapted from RothC‐26.3) was used, coupled with a soil‐redistribution model (LandSoil). SOC dynamics were simulated over 90 years in an agricultural hedgerow landscape dedicated to dairy farming, with a mix of cropping and grasslands. Climate and land use were simulated considering business‐as‐usual scenarios derived from existing information on the study area. A net decrease in SOC stocks was predicted at the end of the simulation period. Soil redistribution induced a net SOC loss equivalent to 2 kg C ha^?1 yr^?1 because of soil exportation out of the study site and an increase in SOC mineralization. Hedgerows and woods were the only land use in which soil redistribution induced net SOC storage. Soil tillage was the main process that induced soil redistribution within cultivated fields. Soil exportation out of the study area was due to erosion by water, but remained low because of the protective role of the hedgerow network. These soil transfers redistributed SOC stocks in the landscape, mostly within cultivated fields. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

Effects of micro-topography on surface–subsurface exchange and runoff generation in a virtual riparian wetland — A modeling study     

S. Frei  G. Lischeid  J.H. Fleckenstein 《Advances in water resources》2010

In humid upland catchments wetlands are often a prominent feature in the vicinity of streams and have potential implications for runoff generation and nutrient export. Wetland surfaces are often characterized by distinct micro-topography (hollows and hummocks). The effects of such micro-topography on surface–subsurface exchange and runoff generation for a 10 by 20 m synthetic section of a riparian wetland were investigated in a virtual modeling experiment. A reference model with a planar surface was run for comparison. The geostatistically simulated structure of the micro-topography replicates the topography of a peat-forming riparian wetland in a small mountainous catchment in South-East Germany (Lehstenbach). Flow was modeled with the fully-integrated surface–subsurface code HydroGeoSphere. Simulation results showed that the specific structure of the wetland surface resulted in distinct shifts between surface and subsurface flow dominance. Surface depressions filled and started to drain via connected channel networks in a threshold controlled process, when groundwater levels intersected the land surface. These networks expanded and shrunk in a spill and fill mechanism when the shallow water table fluctuated around the mean surface elevation under variable rainfall inputs. The micro-topography efficiently buffered rainfall inputs and produced a hydrograph that was characterized by subsurface flow during most of the year and only temporarily shifted to surface flow dominance (> 80% of total discharge) during intense rainstorms. In contrast the hydrograph in the planar reference model was much “flashier” and more controlled by surface runoff. A non-linear, hysteretic relationship between groundwater level and discharge observed at the study site was reproduced with the micro-topography model. Hysteresis was also observed in the relationship between surface water storage and discharge, but over a relatively narrow range of surface water storage values. Therefore it was concluded that surface water storage was a better predictor for the occurrence of surface runoff than groundwater levels.  相似文献   

Miller定理的推论及其在小信号负反馈放大器分析中的应用     

滕军 《成都信息工程学院学报》1988,(2)

本文对电路分析理论中的Miller对定理进行了新的延拓,推导出的另外三个推论使得Miller,定理的应用范围大大地扩展了,它不仅适用于并——并相连的二端对网络分析,而且还适用于串——串相连、并——串相连及串——并相连的二端对网络分析,从而使常规二端对网络的分析更加简化了。从给出的应用举例分析可知,这些推论用于小信号负反馈放大器的分析之中尤其简便。  相似文献   

南京地区高温天气下城市化影响的模拟研究          下载免费PDF全文

马红云  董轩  孙岑霄 《大气科学学报》2018,41(1):67-76

利用WRF(Weather Research and Forecasting)模式耦合单层城市冠层模式,研究了南京地区一次高温热浪过程(2013年8月5—10日)中气溶胶的辐射效应、城市扩张对边界层的影响和它们间的相互作用。结果显示,由于气溶胶的直接辐射效应,在白天,南京近地面温度平均降低约0.11℃,净辐射平均降低约12 W/m~2;城市扩张使近地面温度增加约1.7℃,在本次试验过程中,城市扩张的增暖效应明显强于气溶胶冷却效应。另外,由于城市扩张后产生了较强的增暖作用,加强了周围气流的辐合运动,城市区域风速平均增加约0.8 m/s。白天潜热通量的减少与感热通量的增加导致城市边界层内温度升高,并且城市增暖引起的上升运动将气溶胶抬升至更高层,使边界层更不稳定,气溶胶与城市边界层稳定性之间可能存在正反馈。  相似文献   

Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice     

Yan XIA  Yongyun HU  Jiping LIU  Yi HUANG  Fei XIE  Jintai LIN 《大气科学进展》2020,37(5):505-514

Recent studies demonstrate that the Antarctic Ozone Hole has important influences on Antarctic sea ice.While most of these works have focused on effects associated with atmospheric and oceanic dynamic processes caused by stratospheric ozone changes,here we show that stratospheric ozone-induced cloud radiative effects also play important roles in causing changes in Antarctic sea ice.Our simulations demonstrate that the recovery of the Antarctic Ozone Hole causes decreases in clouds over Southern Hemisphere(SH)high latitudes and increases in clouds over the SH extratropics.The decrease in clouds leads to a reduction in downward infrared radiation,especially in austral autumn.This results in cooling of the Southern Ocean surface and increasing Antarctic sea ice.Surface cooling also involves ice-albedo feedback.Increasing sea ice reflects solar radiation and causes further cooling and more increases in Antarctic sea ice.  相似文献   

大气CO2浓度非均匀分布及其对地表升温影响的研究进展与展望     

张帆  宣鑫  邓祥征 《地球信息科学学报》2021,23(8):1362-1371

在气候变化和全球治理挑战日益严峻的背景下,CO₂排放及代价评估日益受到学术界和决策者的关注。当前全球范围包括联合国政府间气候变化专门委员会（IPCC）评估在内的几乎所有研究都是基于全球平均CO₂浓度来驱动气候模式的,但基于全球CO₂平均分布设定开展模拟影响评估在学术界多有争议。首先,综述了大气CO₂非均匀分布的证据,评述了大气CO₂浓度非均匀分布与地表升温过程的互馈机制。其次,从自然和人为2个维度,梳理了大气CO₂浓度非均匀分布形成的原因,并评估了其对地表升温的影响。最后,评述了当前大气CO₂浓度非均匀分布研究中存在的问题,进一步展望了其发展趋势,为把握全球与区域碳排放现状及气候变化影响提供科学判据。  相似文献