World Map of Natural Hazards – A Global View of the Distribution and Intensity of Significant Exposures     

Berz  G.  Kron  W.  Loster  T.  Rauch  E.  Schimetschek  J.  Schmieder  J.  Siebert  A.  Smolka  A.  Wirtz  A. 《Natural Hazards》2001,23(2-3):443-465

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On the ice age glaciation of the Tibetan highlands and its transformation into a 3-D model     

Prof. Matthias Kuhle Dr.  Klaus Herterich Dr.  R. Calov 《GeoJournal》1989,19(2):201-206

We present an interdisciplinary study on data and modeling intercomparison, concerning the possible existence of a Tibetan ice sheet and its climatological implications during the ice age. In the ice sheet model the fields of ice flow and temperature are calculated, and a highly parameterized formulation of the yearly snow balance is used, defining the forcing at the surface of the ice sheet. The data set used, supplies the height of the equilibrium line of the glaciers (=ELA) and documents the maximum extension of the glaciated areas. With prescribed snow accumulation above the ELA and melting below, the model is integrated for 10 000 model years and the model glaciation is then compared with the data.The main results are: Provided the height of the glacial equilibrium line has been reconstructed correctly, a Tibetan ice sheet can be bult up within 10 000 model years, using moderate rates of precipitation (maximum snow fall: 100 mm/year). Comparison of data and model glaciation suggests an increase of precipitation from the NW to the E of Tibet and from the S to the NE, which reflects the presently observed pattern of the monsoon circulation.  相似文献   

The spatial variability of Amazonian soils under natural forest and pasture     

José C. Correa  Prof. Dr. Klaus Reichardt 《GeoJournal》1989,19(4):423-427

Spatial variability of physical and chemical properties in Amazonian soils is evaluated on sites of natural rain forest and pastures of different age in the Amazon region. The sampling scheme was regionalized using transects of fifty points 3 m apart each. Variables analysed were: soil bulk density; resistance to penetration; soil water content; available water; pH and extractable ions such as Ca, K, Al, P and Zn. Geostatistical analyses show that most variables are space independent for the 3 m spacing used. Variances indicate a much lower variability of the measured properties in the forest as compared to pastures.  相似文献   

Gravity interpretation of a unified 2-D acoustic image of the central Alpine collision zone   总被引：1，自引：0，他引：1  

Klaus Holliger  Edi Kissling 《Geophysical Journal International》1992,111(2):213-225

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Announcements     

Stephan Schuhmann  Klaus Herrmann  Kurt Rothermel  Jan Blumenthal  Dirk Timmermann 《Stochastic Hydrology and Hydraulics》1993,7(1):83

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Neuere Veröffentlichungen     

Klaus Figge 《Ocean Dynamics》1993,45(1):55-56

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Seismic structure of gneissic/granitic upper crust: geological and petrophysical evidence from the Strona-Ceneri Zone (northern Italy) and implications for crustal seismic exploration   总被引：2，自引：0，他引：2  

Klaus Holliger  Alan Levander 《Geophysical Journal International》1994,119(2):497-510

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The Chassigny meteorite: a cumulate dunite with hydrous amphibole-bearing melt inclusions     

R.J. Floran  Martin Prinz  P.F. Hlava  Klaus Keil  C.E. Nehru  J.R. Hinthorne 《Geochimica et cosmochimica acta》1978,42(8):1213-1229

The Chassigny meteorite is a moderately shocked olivine achondrite or chassignite with features indicative of a cumulate origin with some subsolidus annealing. Chassigny is an iron-rich dunite (Fo₆₈) with minor amounts of Ca-rich and Ca-poor pyroxene, alkalic feldspar, chromite, and melt inclusions in olivine. Accessory phases include chlorapatite, troilite, marcasite, kaersutite amphibole, pentlandite, ilmenite, rutile and baddeleyite. The meteorite experienced shock pressures of ~150–200 kbar as evidenced by planar and irregular fractures in olivine, local recrystallization in pyroxene and reduced birefringence and rare deformation lamallae in feldspar. Kaersutitic amphibole (K_0.05 Na_0.45)_0.50 (Ca_1.71 Na_0.29)_2.00 (Mg_2.73 ‘Fe’_1.19 Ti_0.73 A1_0.23 Cr_0.08 Mn_0.03)_4.99 (Si_6.05Al_1.95)_8.00 O₂₂ (OH, F)₂ containing hydrogen and lesser amounts of fluorine represents the first extraterrestrial occurrence of hydrous amphibole and the first meteoritic amphibole type other than fluorichterite. Kaersutite is found only in melt inclusions.Melt inclusion bulk compositional data suggest crystallization from a low-Ca melt that may have been similar in major element abundances to the silicate portion of LL group chondrites. However, Chassigny has a fractionated pattern for REE and the lack of metallic iron, possible presence of minor Ni in the olivine and Fe³⁺ in the chromites indicates that Chassigny formed under relatively more oxidizing conditions than most other achondrites. Therefore its parental melt could not have been directly derived from a chondritic composition in a simple single-stage process. The iron-rich bulk composition, cumulate texture and abundance as well as alkalic nature of the interstitial feldspar indicate that Chassigny could not have generated eucritic magmas. This places further constraints on its relationship to other meteorites and the parent body from which it is derived. The Brachina meteorite is similar to Chassigny except that it is finer grained, more feldspathic and is unshocked. It extends the fractionation range of this group which now represents two unusual meteorites.  相似文献   

Der Einfluß des Windes auf die Wasserbewegungen durch die Straße von Dover     

Klaus Wyrtki 《Ocean Dynamics》1952,5(1):21-27

Zusammenfassung Es werden die Beziehungen zwischen den über der südlichen Nordsee herrschenden Winden und den durch die Straße von Dover stattfindenden Wasserbewegungen abgeleitet. Diese werden einerseits durch den unmittelbaren Windeinfluß und andererseits durch das im wesentlichen auch windbedingte Gefälle vom Kanal zur Nordsee bestimmt. Der Jahresgang und im Zusammenhang damit das Vorrücken salzreichen Wassers im Kanal werden untersucht. Die bei Feuerschiff Varne auftretenden Richtungsänderungen des mittleren jährlichen Reststromes werden durch Schwankungen der Windgeschwindigkeit erklärt. An Hand von Salzgehaltskarten aufeinanderfolgender Monate werden Bewegungen von Wasserkörpern und Fronten im Kanal unter dem Einfluß des Windes verfolgt. Auf die Bedeutung solcher Untersuchungen synoptischer Art zum Studium der Wasserbewegungen wird hingewiesen.

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The wind's influence on the flow of water through the Straits of Dover

Summary The relations between the winds blowing over the southern North Sea and the flow of water through the Straits of Dover are derived; this flow of water depends on both the immediate influence of the wind and the slope of the sea surface between the Channel and the North Sea which, too, is mainly produced by the wind. The annual variation and, in connection with it, the advance of Atlantic water into the Channel are investigated. The changes of directions the mean annual residual current is subjected to according to the observations made near the light vessel Varne are found to be due to variations in the wind velocity. The shifting of water bodies and fronts in the Channel as dependent on the wind is studied by means of salinity charts over consecutive months. Finally, attention is drawn to the significance of such synoptical investigations for the study of water movements.

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L'influence du vent sur les mouvements de l'eau dans le Pas de Calais

Résumé Les relations entre les vents dominant au sud de la mer du Nord et les mouvements de l'aeu dans le Pas de Calais sont dérivées. Ces mouvements sont causés par l'action immédiate du vent ainsi que par la pente de la surface entre la Manche et la mer du Nord; celle-ci, de sa part, est de même essentiellement causée par le vent. La marche annuelle et, en conséquence, la progression de l'eau atlantique dans la Manche sont étudiées. Les changements de direction du courant résiduel moyen par an dérivés des observations du bateau feu Varne sont expliqués en fonction des changements de vitesse du vent. À l'aide des cartes de salinité sur des mois consécutifs les mouvements des masses d'eau et des fronts dans la Manche sont étudiés par rapport à leur dépendance du vent. En résumé, l'attention est attirée sur l'importance de telles investigations synoptiques pourl'étude des mouvements de l'eau.

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An Unusual Bluegreen Alga Symbiotic with Two New Species of Ulosa (Porifera: Hymeniacidonidae) from Carrie Bow Cay,Belize*     

Klaus Rützler 《Marine Ecology》1981,2(1):35-50

Abstract. Two new species of the sponge genus Ulosa were found living in symbiosis with a chroococcacean cyanophyte (cyanobacterium) in shallow Caribbean coral reefs off Belize (Central America). Ulosa funicularis is a stringy green sponge (styles: 157 × 2.5 μm, mean dimensions); U. arenosa is a thickly encrusting, shaggy, brownish-greenish mottled species with sandy ectosome (styles: 175 × 3.6 μm). The endosymbiotic algae make up 50% of the cellular sponge tissue. The algal cells are light green, spherical, 5–9 μm in diameter, and divide by median constriction. Electron microscopy shows that cell walls are fully developed but that thylakoids are unusual for their inflated sacs, which are in communication with the nucleoplasmic regions. Although the pigment composition is typical for the Cyanophyta, the phycobiliproteins occur in considerably  相似文献