START — the road from Bellagio     

Roland J Fuchs 《Global Environmental Change》1995,5(5)

The START initiative (co-sponsored by IGBP, WCRP and HDP) has as its primary objective development of regional frameworks to support regional research related to global change, associated capacity building and synthesis scientific assessments related to policy development. START now has six regional networks under development in South-East Asia, Northern Africa, East Asia, South Asia, the Meditteranean, and Southern Africa. Issues before START include the coordination of regional activities with that of sponsoring programmes, the need for a more elaborated HDP, and the development of thematic programming that will secure multi-donor, multi-year support.  相似文献   

Massif Central (France): new constraints on the geodynamical evolution from teleseismic tomography   总被引：2，自引：0，他引：2  

M. Granet  G. Stoll  J. Dorel  U. Achauer  G. Poupinet  K. Fuchs 《Geophysical Journal International》1995,121(1):33-48

The Massif Central, the most significant geomorphological unit of the Hercynian belt in France, is characterized by graben structures which are part of the European Cenozoic Rift System (ECRIS) and also by distinct volcanic episodes, the most recent dated at 20 Ma to 4000 years BP. In order to study the lithosphere-asthenosphere system beneath this volcanic area, we performed a teleseismic field experiment.
During a six-month period, a joint French-German team operated a network of 79 mobile short-period seismic stations in addition to the 14 permanent stations. Inversion of P -wave traveltime residuals of teleseismic events recorded by this dense array yielded a detailed image of the 3-D velocity structure beneath the Massif Central down to 180 km depth. The upper 60 km of the lithosphere displays strong lateral heterogeneities and shows a remarkable correlation between the volcanic provinces and the negative velocity perturbations. The 3-D model reveals two channels of low velocities, interpreted as the remaining thermal signature of magma ascent following large lithospheric fractures inherited from Hercynian time and reactivated during Oligocene times. The teleseismic inversion model yields no indication of a low-velocity zone in the mantle associated with the graben structures proper. The observation of smaller velocity perturbations and a change in the shape of the velocity pattern in the 60–100 km depth range indicates a smooth transition from the lithosphere to the asthenosphere, thus giving an idea of the lithosphere thickness. A broad volume of low velocities having a diameter of about 200 km from 100 km depth to the bottom of the model is present beneath the Massif Central. This body is likely to be the source responsible for the volcanism. It could be interpreted as the top of a plume-type structure which is now in its cooling phase.  相似文献   

Micro-sized enterprises: vulnerability to flash floods     

Konstantinos Karagiorgos  Micha Heiser  Thomas Thaler  Johannes Hübl  Sven Fuchs 《Natural Hazards》2016,81(2):1091-1106

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XXIII INTERNATIONAL GEOGRAPHICAL CONGRESS,U.S.S.R.     

Roland J. Fuchs 《The Professional geographer》1977,29(3):296-297

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Comparison of Dimensionless Parameters in Astrophysical MHD Systems and in Laboratory Experiments     

E. P. Kurbatov  D. V. Bisikalo  M. V. Starodubtsev  A. Ciardi  J. Fuchs  A. A. Solov’ev  K. F. Burdonov  G. Revet  S. Chen 《Astronomy Reports》2018,62(8):483-491

Estimates of typical parameters of accretion flows in the representative intermediate polar EX Hydrae, the polar AM Herculis, and the “hot Jupiter” WASP-12b are presented. Dimensionless parameters of astrophysical systems are compared with those of laboratory experiments on laser ablation in magnetic fields. It is shown that laboratory simulations of astrophysical flows is possible in principle, provided that some adjustment to the magnetic field, plasma density, and plasma velocity are made.  相似文献   

On self–killing and self–creating dynamos     

H. Fuchs  K.-H. Rdler  M. Rheinhard 《Astronomische Nachrichten》1999,320(3):129-133

Numerical studies with a spherical dynamo model have shown two remarkable phenomena. The model consists of a spherical body of an electrically conducting incompressible uid surrounded by free space. In addition to a rotation of the body an inner motion due to a given forcing is considered which satisfies a no–slip condition at the boundary. The full interaction of magnetic field and motion is taken into account. Starting from a fluid motion capable of dynamo action and a very weak magnetic field it was observed that the growing magnetic field destroys the dynamo property of the motion and then decays, and that the system ends up in a state with another motion incapable of dynamo action and zero magnetic field. In another case with a motion unable to prevent small magnetic fields from decay it proved to be possible that stronger magnetic fields deform it so that a dynamo starts to work which enables the system to approach a steady state with a finite magnetic field.  相似文献   

The adoption of best management practices to reduce agricultural water contamination   总被引：2，自引：0，他引：2  

T.J. Centner  J.E. Houston  A.G. Keeler  C. Fuchs   《Limnologica》1999,29(3):366

Nonpoint source water pollution generated by agricultural production is considered a major environmental issue in the United States and Europe. One strategy in the United States has been to adopt various measures, called best management practices (BMPs), to reduce water pollution. Our research addresses legal institutions and the applied use of BMPs, and discusses compensatory payments to reduce nitrogen fertilization levels. Models employed in Georgia and Baden-Wuerttemberg evaluate institutional constraints of payments to reduce nitrogen usage, penalties for excessive leaching, and financial incentives for meeting minimum mineralized nitrogen levels. By modeling net returns, preferred economic strategies for producers are identified. Results show that while BMPs can reduce agricultural nonpoint contamination, pollution abatement may be costly to producers. Thus, reduced pollution probably will require some type of government intervention.  相似文献   

GOCE gravitational gradients along the orbit   总被引：6，自引：3，他引：3  

Johannes Bouman  Sophie Fiorot  Martin Fuchs  Thomas Gruber  Ernst Schrama  Christian Tscherning  Martin Veicherts  Pieter Visser 《Journal of Geodesy》2011,85(11):791-805

GOCE is ESA’s gravity field mission and the first satellite ever that measures gravitational gradients in space, that is, the second spatial derivatives of the Earth’s gravitational potential. The goal is to determine the Earth’s mean gravitational field with unprecedented accuracy at spatial resolutions down to 100 km. GOCE carries a gravity gradiometer that allows deriving the gravitational gradients with very high precision to achieve this goal. There are two types of GOCE Level 2 gravitational gradients (GGs) along the orbit: the gravitational gradients in the gradiometer reference frame (GRF) and the gravitational gradients in the local north oriented frame (LNOF) derived from the GGs in the GRF by point-wise rotation. Because the V _XX , V _YY , V _ZZ and V _XZ are much more accurate than V _XY and V _YZ , and because the error of the accurate GGs increases for low frequencies, the rotation requires that part of the measured GG signal is replaced by model signal. However, the actual quality of the gradients in GRF and LNOF needs to be assessed. We analysed the outliers in the GGs, validated the GGs in the GRF using independent gravity field information and compared their assessed error with the requirements. In addition, we compared the GGs in the LNOF with state-of-the-art global gravity field models and determined the model contribution to the rotated GGs. We found that the percentage of detected outliers is below 0.1% for all GGs, and external gravity data confirm that the GG scale factors do not differ from one down to the 10⁻³ level. Furthermore, we found that the error of V _XX and V _YY is approximately at the level of the requirement on the gravitational gradient trace, whereas the V _ZZ error is a factor of 2–3 above the requirement for higher frequencies. We show that the model contribution in the rotated GGs is 2–35% dependent on the gravitational gradient. Finally, we found that GOCE gravitational gradients and gradients derived from EIGEN-5C and EGM2008 are consistent over the oceans, but that over the continents the consistency may be less, especially in areas with poor terrestrial gravity data. All in all, our analyses show that the quality of the GOCE gravitational gradients is good and that with this type of data valuable new gravity field information is obtained.  相似文献   

A quantitative vulnerability function for fluvial sediment transport   总被引：11，自引：6，他引：5  

Reinhold Totschnig  Walter Sedlacek  Sven Fuchs 《Natural Hazards》2011,58(2):681-703

In quantitative risk assessment, risk is expressed as a function of hazard, elements at risk exposed, and vulnerability. Vulnerability is defined as the expected degree of loss for an element at risk as a consequence of a certain event, following a natural-scientific approach combined with economic methods of loss appraisal. The resulting value ranges from 0 (no damage) to 1 (complete destruction). With respect to torrent processes, i.e., fluvial sediment transport, this concept of vulnerability—though widely acknowledged—did not result in sound quantitative relationships between process intensities and associated degrees of loss so far, even if considerable loss occurred during recent years. To close this gap and establish this relationship, data from three well-documented torrent events in the Austrian Alps were used to derive a quantitative vulnerability function applicable to residential buildings located on torrent fans. The method applied followed a spatially explicit empirical approach within a GIS environment and was based on process intensities, the spatial characteristics of elements at risk, and average reconstruction values on a local scale. Additionally, loss data were collected from responsible administrative bodies and analysed on an object level. The results suggest a modified Weibull distribution to fit best to the observed damage pattern if intensity is quantified in absolute values, and a modified Frechet distribution if intensity is quantified relatively in relation to the individual building height. Additionally, uncertainties resulting from such an empirical approach were studied; in relation to the data quality a 90% confidence band was found to represent the data range appropriately. The vulnerability relationship obtained allows for an enhanced quantification of torrent risk, but also for an inclusion in comprehensive vulnerability models including physical, social, economic, and institutional vulnerability. As a result, vulnerability to mountain hazards might decrease in the future.  相似文献   

Infrared measurement of canopy temperature and detection of plant water stress   总被引：9，自引：0，他引：9  

M. Fuchs 《Theoretical and Applied Climatology》1990,42(4):253-261

Summary Leaf temperature is directly determined by leaf energy and water balance. If diminished water availability decreases latent heat flux at the leaf surface, a complementary increase of sensible heat will occur and create a larger temperature difference between foliage and air. Radiation, air temperature, humidity and wind speed modify leaf temperature and may mask indications of water stress. The position, inclination and orientation of leaves within the canopy also produce considerable variation of leaf temperature. These factors were incorporated in a linear transpiration model, using physical and physiological characteristics of cotton. Water stress was simulated by imposing a limit value for stomatal conductance. The energy balance equation was solved as a function of angle between leaf and solar beam, to determine leaf temperature frequency distribution. The results show that stress induced temperature rise occurs over a small percentage of the total leaf area. Detection of moderate stress requires a normalizing procedure which takes into account meteorological conditions. The leaf temperature distribution is a better indicator of stress than the average value.The infrared thermometer integrates thermal radiation emitted by the foliage included in its field of view. The model simulated the temperature composition of the field of view as a function of sighting angle and orientation relative to the incident solar beam. The spatial averaging of the signal in the field of view, attenuated the sensitivity of the measurement to water stress. The results also indicated that pointing the infrared thermometer towards the canopy in the same direction as the sun, and at an angle of incidence as close as possible to the solar zenith angle, improved the ability to detect water stress.Contribution from the Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel. No. 2638-E, 1989 series. This work was supported by grant No. US-1138-86 from the Binational Agricultural Research and Development Fund.With 9 Figures  相似文献