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921.
This paper deals with numerical experiments based on the coupled ECHAM-HOPE model. The results of experiments are analyzed.
The initial fields for the calculations over time periods from one month to one year are constructed based on the results
of the data assimilation of temperature profiles from TOGA-TAO moorings. The perturbations of the initial fields and the propagation
of these perturbations with specific computational time intervals are analyzed on the basis of the results of these experiments.
It is shown that the strongest impacts of the perturbations are localized in specific regions of the World Ocean corresponding
to the energetically active zones of the Earth. The mechanism of the transition of these perturbations is also studied. Different
statistical properties of the ensemble of experiments are presented. 相似文献
922.
The trophic position of Calanus finmarchicus in the Trondheim Fjord in 2004 was determined through stable isotope analyses. Wild specimens were sampled monthly in the fjord and δ13C and δ15N signatures of the developmental stages from CIII to adults were measured. There were statistically significant differences in the δ13C and δ15N signatures of three identified groups: overwintered parental generation, developing new generation and new generation preparing for overwintering. C. finmarchicus individuals raised in a laboratory on a pure algal diet (Dunaliella tertiolecta and Isochrysis galbana) provided stable isotope signatures for purely herbivorous copepods. With these signatures as comparison, the trophic position of C. finmarchicus in the Trondheim Fjord in 2004 was determined as trophic level 2.4, thus indicating omnivory under natural conditions. Additionally, our data suggest that seasonal differences in the δ13C signatures of C. finmarchicus are due to the varying lipid content of the different developmental stages. 相似文献
923.
K. K. I. U. Arunakumara ZHANG Xuecheng 《中国海洋大学学报(英文版)》2008,7(1):60-64
924.
现行黄河口水下三角洲海底形貌及不稳定性 总被引:4,自引:0,他引:4
杨作升 G.H.Keller 陆念祖 D.B.Prior 林天充 B.D.Bornhold 许卫东 L.D.Wright J.Suhayda 曹立华 W.J.Wisenman 《中国海洋大学学报(自然科学版)》1990,(1)
高分辨力的声学仪器调查表明,现行黄河口水下三角洲海底的形貌十分复杂,由于高浓度巨量黄河泥沙快速沉积的结果,使河口底坡出现了大量的不稳定性现象,如塌陷冲沟,高密度沉积物重力流,切割—充填结构海底,V形水下河谷、滑塌等。根据海底扰动程度作了分区,划分了地形单元,并对不同的海底形态的成因作了分析。比较了1985和1986年两个航次考查结果的变动,分析了原因。 相似文献
925.
Thiele A. Cadario E. Schulz K. Soergel U. 《Geoscience and Remote Sensing Letters, IEEE》2010,7(1):83-87
926.
Interaction of Aquatic Dissolved Organic Matter(DOM) with Amitrole: The Nature of the Bound Residues
In this study the binding behaviour of the herbicide amitrole with humic substances respectively dissolved organic matter (DOM) is presented. The results of the binding and release experiments using radio actively 14C-labelled amitrole ledto the conclusion that the binding of amitrole is very low. About 70% of amitrole bound to humic substances was not extractable. The releasable amitrole portion of the purified DOM-amitrolecomplexes led to a harmful effect in the cress test. Solid-state cross polarisation (CP) magic angle spinning (MAS) 15N-NMR spectroscopy is a powerful spectroscopic method to elucidate the structure of bound xenobiotics. In addition extraction experiments were used resulting in a binding scheme of amitrole to DOM, where above all the covalent bonding occurred via acid amide bonds. 相似文献
927.
M. I. Wilkinson A. Vallenari C. Turon U. Munari D. Katz G. Bono M. Cropper A. Helmi N. Robichon F. Thévenin S. Vidrih T. Zwitter F. Arenou M.-O. Baylac G. Bertelli A. Bijaoui F. Boschi F. Castelli F. Crifo M. David A. Gomboc A. Gómez M. Haywood U. Jauregi P. de Laverny Y. Lebreton P. Marrese T. Marsh S. Mignot D. Morin S. Pasetto M. Perryman A. Pra A. Recio-Blanco F. Royer A. Sellier A. Siviero R. Sordo C. Soubiran L. Tomasella Y. Viala 《Monthly notices of the Royal Astronomical Society》2005,359(4):1306-1335
928.
S. Mischke U. Herzschuh C. Zhang J. Bloemendal F. Riedel 《Global and Planetary Change》2005,46(1-4):337
Two sediment cores (length 13.94 and 12.93 m) have been drilled from the small alpine Lake Luanhaizi in the eastern central Qilian Mountains and correlated by means of magnetic susceptibility (MS). This paper focuses on the lithology and chronology of the longer core, on the results of loss on ignition (LOI), element concentration, thermomagnetic as well as magnetic hysteresis loop measurements, and on the ostracod record.The recovered sediments represent three types of depositional environment: a shallow intermittent lake, a deeper permanent lake and a true playa lake. Three stages of a higher lake level and permanence of the water body are reconstructed. The lowermost stage of a permanent lake and inferred favourable environmental conditions occurred probably about 45 14C ka BP. The second stage of a deeper permanent lake occurred either shortly before or, more likely, following the LGM. Most favourable environmental conditions and highest water levels were reconstructed for the uppermost stage comprising the Holocene. Considering the lake record, glaciers have not reached the lake site at 3200 m altitude during the LGM, providing further evidence against a large ice sheet on the Tibetan Plateau. 相似文献
929.
To be able to simulate the interaction of extrasolar planets with the stellar wind, a number of planetary parameters are required. Some of these (like planetary mass and radius) can be obtained directly from observational data. Other properties are not known very precisely. For example, up to now, there is no observation providing information on the strength of planetary magnetic moments. However, there is good reason to expect only very small magnetic moments for planets in very close orbits around their stars (like HD 209458 b and OGLE-TR-56 b). Thus, as a first step towards a more complete treatment, it seems reasonable to treat the interaction of the stellar wind with an unmagnetized planet. Calculations were performed for a nonconducting as well as for a weakly conducting planet. The interaction with the stellar wind and the resulting induced magnetosphere was simulated using a three dimensional hybrid code as well as in the drift-kinetic approximation. The effect of a interplanetary magnetic field oriented perpendicular to the incoming stellar wind was included. In the case of a weakly conducting body an asymmetrical Mach cone is formed, whereas for a nonconducting body no Mach cone is observed. These investigations will serve as the first step in the search for particular effects occurring at extrasolar planets, which could possibly lead to observable effects, e.g. radio emission. The results are also relevant for plasma structures near weakly conducting, unmagnetized bodies like the Earth's moon. 相似文献
930.
VINCENT R. RINTERKNECHT LESZEK MARKS JAN A. PIOTROWSKI GRANT M. RAISBECK FRANÇOISE YIOU EDWARD J. BROOK PETER U. CLARK 《Boreas: An International Journal of Quaternary Research》2005,34(2):186-191
Rinterknecht, V. R., Marks, L., Piotrowski, J. A., Raisbeck, G. M., Yiou, F., Brook, E. J. & Clark, P. U. 2005 (May): Cosmogenic 10 Be ages on the Pomeranian Moraine, Poland. Boreas , Vol. 34, pp. 186–191. Oslo. ISSN 0300–9483.
We measured the10 Be concentrations in boulders collected from the Pomeranian Moraine in Poland, providing the first direct dating of the southern margin of the Scandinavian Ice Sheet (SIS) in the Polish Lowland. The mean age of 8 10 Be ages of the Pomeranian Moraine in northwestern Poland is 14.30.8 10 Be ka, while in northeastern Poland the mean age of 19 10 Be ages of the moraine is 15.00.5 10 Be ka. Given the excellent agreement between the two age groups, we calculate a mean age of 14.80.4 10 Be ka for final deposition of the Pomeranian Moraine of northern Poland. The age of the Pomeranian Moraine suggests that the southern margin of the SIS was near its maximum extent in Poland at a younger time than previously inferred, and that retreat from the moraine at 14.80.4 10 Be ka probably occurred in response to the onset of the Bølling interstade. 相似文献
We measured the