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Li-Cai Deng Heidi Jo Newberg Chao Liu Jeffrey L. Carlin Timothy C. Beers Li Chen Hsu-Tai Lee Carl J. Grillmair Puragra Guhathakurta Zhan-Wen Han Jin-Liang Hou Sebastien Lepine Jing Li Xiao-Wei Liu Kai-Ke Pan J. A. Sellwood Bo Wang Hong-Chi Wang Fan Yang Brian Yanny Hao-Tong Zhang Yue-Yang Zhang Zheng Zheng Zi Zhu 《天体物理学报》2012,(7):735-754
43.
Jeffrey L. Carlin Sebastien Lepine Heidi Jo Newberg Li-Cai Deng Timothy C. Beers Yu-Qin Chen Norbert Christlie Xiao-Ting Fu Shuang Gao Carl J. Grillmair PuragraGuhathakurta Zhan-Wen Han Jin-Liang Hou Hsu-Tai Lee Jing Li Chao Liu Xiao-Wei Liu Kai-Ke Pan J. A. Sellwood Hong-Chi Wang Fan Yang Brian Yanny Yue-Yang Zhan Zheng Zheng Zi Zhu 《天体物理学报》2012,(7):755-771
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Coping with floods in the city of Dresden,Germany 总被引:5,自引:2,他引:3
During August 2002 and again in March 2005 as well as in April 2006 the city of Dresden was hit by floods. The flood in 2002
was an extreme event, only comparable to flooding in 1862 and 1890 in Dresden. The flood discharge in 2006 was the second
highest discharge since 1940 at the Dresden gauge although its return period was only about 15 years. This special situation
enables a comparison of the preparedness of authorities and households in the flood endangered city of Dresden in 2002 after
a long period of relatively low flood discharges and in 2005/2006 just a few years after a severe flood event. Before August
2002, the flood risk awareness and flood preparedness of authorities and households in Dresden was low. The inundation channels
and the Elbe riverbed had not been maintained well. Just 13% of the households had undertaken building precautionary measures.
The severe flood situation as well as the low flood preparedness led to tremendous damage, e.g., losses to residential buildings
amounted to 304 million €. After 2002, the municipal authorities in Dresden developed a new flood management concept and many
households were motivated to undertake precautionary measures. Building precautionary measures had been actually undertaken
by 67% of the households before the floods in 2005 and 2006. Flood damage was significantly lower, due to the less severe
flood situations and the much better preparedness. It is an important challenge for the future to keep preparedness at a high
level also without recurrent flood experiences. 相似文献
46.
One of the most documented effects of human activity on our environment is the reduction of stratospheric ozone resulting
in an increase of biologically harmful ultraviolet (UV) radiation. In a less predictable manner, UV radiation incident at
the surface of the earth is expected to be further modified in the future as a result of altered cloud condition, atmospheric
aerosol concentration, and snow cover. Although UV radiation comprises only a small fraction of the total solar radiation
that is incident at the earth’s surface, it has the greatest energy per unit wavelength and, thus, the greatest potential
to damage the biosphere. Recent investigations have highlighted numerous ways that UV radiation could potentially affect a
variety of ecological processes, including nutrient cycling and the terrestrial carbon cycle. The objectives of the following
literature review are to summarize and synthesize the available information relevant to the effects of UV radiation and other
climate change factors on the terrestrial carbon balance in an effort to highlight current gaps in knowledge and future research
directions for UV radiation research. 相似文献
47.
Heidi E. Kretser Elliot Dale Leslie Karasin Liba Pejchar Sarah E. Reed 《社会与自然资源》2019,32(9):1021-1039
Conservation Development (CD) is a land-use tool to reduce the impacts of development on natural resources, yetthe use of CD is highly variable. We used a collaborative conservation model to examine factors influencing adoption and implementation to improve the future application of CD. We interviewed 2–3 individuals including planners, board members, and developers (n?=?46) from 16 rural communities in the intermountain west and northeast U.S. Motivations to preserve rural character or comply with state statutes drove adoption. Greater capacity such as outside expertise, model regulations, and iterative revisions of ordinances was associated with stronger ordinances. Adoption processes including ample dialog across diverse constituents, especially those overseeing subdivision development, facilitated higher rates of implementation. Concerns over open space management, lack of successful CD examples, and inexperience with CD posed barriers to implementation. Understanding social context revealed the strengths and shortcomings of CD and provided guidance for strategically engaging communities in private lands conservation. 相似文献
48.
Employing the properties of the affine mappings, a very novel fractal model scheme based on the iterative function system is proposed. We obtain the vertical scaling factors by a set of the middle points in each affine transform, solving the difficulty in determining the vertical scaling factors, one of the most difficult challenges faced by the fractal interpolation. The proposed method is carried out by interpolating the known attractor and the real discrete sequences from seismic data. The results show that a great accuracy in reconstruction of the known attractor and seismic profile is found, leading to a significant improvement over other fractal interpolation schemes. 相似文献
49.
Successful species conservation typically results in conflicts between wildlife protection and economic uses of natural resources as in fisheries and aquaculture. This article shows why managing these conflicts require a more comprehensive approach than currently pursued by endangered species conservation programmes. Against the background of several case studies focussing on wildlife conflicts in European waters this article derives two challenges for institutional response: First, the question of mandate—which societal actor initiates management related processes that require multiple actors to collaborate? Second, how can continuous processes of collaboration be sustained? 相似文献
50.
Heidi Houston Helen Anderson Susan L. Beck Jiajun Zhang Susan Schwartz 《Pure and Applied Geophysics》1993,140(2):331-364
To evaluate the tectonic significance of the October 20, 1986 Kermadec earthquake (M
w
=7.7), we performed a comprehensive analysis of source parameters using surface waves, body waves, and relocated aftershocks. Amplitude and phase spectra from up to 93 Rayleigh waves were inverted for centroid time, depth, and moment tensor in a two-step algorithm. In some of the inversions, the time function was parameterized to include information from the body-wave time function. The resulting source parameters were stable with respect to variations in the velocity and attenuation models assumed, the parameterization of the time function, and the set of Rayleigh waves included. The surface wave focal mechanism derived (=275°, =61°, =156°) is an oblique-compressional mechanism that is not easy to interpret in terms of subduction tectonics. A seismic moment of 4.5×1020 N-m, a centroid depth of 45±5 km, and a centroid time of 13±3 s were obtained. Directivity was not resolvable from the surface waves. The short source duration is in significant contrast to many large earthquakes.We performed a simultaneous inversion ofP andSH body waves for focal mechanism and time function. The focal mechanism agreed roughly with the surface wave mechanism. Multiple focal mechanisms remain a possibility, but could not be resolved. The body waves indicate a short duration of slip (15 to 20 s), with secondary moment release 60s later. Seismically radiated energy was computed from the body-wave source spectrum. The stress drop computed from the seismic energy is about 30 bars. Sixty aftershocks that occurred within three months of the mainshock were relocated using the method of Joint Hypocentral Determination (JHD). Most of the aftershocks have underthrusting focal mechanisms and appear to represent triggered slip on the main thrust interface. The depth, relatively high stress drop, short duration of slip, and paucity of true aftershocks are consistent with intraplate faulting within the downgoing plate. Although it is not clear on which nodal plane slip occurred, several factors favor the roughly E-W trending plane. The event occurred near a major segmentation in the downgoing plate at depth, near a bend in the trench, and near a right-lateral offset of the volcanic are by 80 km along an E-W direction. Also, all events in the region from 1977 to 1991 with CMT focal mechanisms similar to that of the Mainshock occurred near the mainshock epicenter, rather than forming an elongate zone parallel to the trench as did the aftershock activity. We interpret this event as part of the process of segmentation or tearing of the subducting slab. This segmentation appears to be related to the subduction of the Louisville Ridge, which may act as an obstacle to subduction through its buoyancy. 相似文献