作者: 最小 時(shí)間: 2025-3-29 05:34
M. Hugi,J. Lang,R. Müller,J. Sromicki,L. Jarczyk,A. Strza?kowski,H. Wita?a,K. A. Eberhardt techniques employing sediment traps using a polyvinyl chloride pipe to capture suspended sediment and a handheld analyzer for X-ray fluorescent analysis and a digital scanner for image analysis were employed for sediment measurement and analysis. In laboratory experiments, the sediment catch perfo
作者: Initial 時(shí)間: 2025-3-29 10:31
作者: 細(xì)查 時(shí)間: 2025-3-29 13:25
G. Gaul,W. Bickel,W. Lahmer,R. Santobservational and numerical frameworks. Shirahama Bay with shallower water and Funauki Bay with deeper water in the northwestern part of Iriomote Island?are mutually connected by a channel. Tidal flows in both bays are expected to be much more complex than those of Sakiyama and Amitori bays, discusse
作者: 細(xì)頸瓶 時(shí)間: 2025-3-29 17:20
K. M. Hartmann,W. Dünnweber,W. E. Frahnbservational and numerical frameworks. Shirahama Bay with shallower water and Funauki Bay with deeper water in the northwestern part of Iriomote Island?are mutually connected by a channel. Tidal flows in both bays are expected to be much more complex than those of Sakiyama and Amitori bays, discusse
作者: Picks-Disease 時(shí)間: 2025-3-29 21:15
作者: libertine 時(shí)間: 2025-3-30 01:10
作者: Herbivorous 時(shí)間: 2025-3-30 06:18
E. R. Cosman,R. J. Ledoux,M. J. Bechara,C. E. Ordonez,H. A. Al-Juwaird the physical environment.Provides detailed information for.This book presents recent results of collaborative studies in geophysics and ecology, focusing on the relationship between the physical environment and the distribution of the marine coastal ecosystems. The study area, the Sakiyamawan–Amit
作者: Hallmark 時(shí)間: 2025-3-30 11:38
K. Katori,K. Furuno,J. Schimizu,Y. Nagashima,S. Hanashima,M. Satot techniques employing sediment traps using a polyvinyl chloride pipe to capture suspended sediment and a handheld analyzer for X-ray fluorescent analysis and a digital scanner for image analysis were employed for sediment measurement and analysis. In laboratory experiments, the sediment catch perfo
作者: 笨重 時(shí)間: 2025-3-30 13:25
D. Konnerth,K. G. Bernhardt,K. A. Eberhard,R. Singh,A. Strzalkowski,W. Trautmann,W. Trombikweak, almost everywhere, when compared with the Coriolis acceleration and the pressure gradient. Friction rarely upsets the geostrophic balance to lowest order. Indeed, for many flows it is probably also true that the dissipative time scale is long compared to the advective time scale, i.e., that th
作者: 一大群 時(shí)間: 2025-3-30 20:11
作者: overshadow 時(shí)間: 2025-3-30 23:44
W. Hoppe,E. Klau?,D. Sprengel,J. Drevermann,R. Isenbügel,H. v. Buttlar,N. Marquardt The radiant energy emitted by the sun may vary somewhat over very long periods, but a sensible idealization for most meteorological and oceanographic purposes consists in considering the solar source strength as fixed. Temporal variations in the incident radiation (and its spatial distribution) are
作者: 跟隨 時(shí)間: 2025-3-31 03:48
作者: BABY 時(shí)間: 2025-3-31 06:50
作者: 狂熱文化 時(shí)間: 2025-3-31 10:36
作者: MUT 時(shí)間: 2025-3-31 15:09
S.T. Thorntonatics and dynamics as influenced by earth’s rotation. Its didactic value is based on elaborate treatment of basic principles, derived equations, exemplary solutions and their interpretation..Both starting graduate students and experienced scientists can closely follow the mathematical development of
作者: 愚蠢人 時(shí)間: 2025-3-31 21:01
作者: 從容 時(shí)間: 2025-3-31 23:52
J. P. Schifferng blocks.Explains derived equations and re-interprets theirThis book develops a fundamental understanding of geophysical fluid dynamics based on a mathematical description of the flows of inhomogeneous fluids.?It covers these topics:.1. development of the equations of motion for an inhomogeneous fl
作者: 不怕任性 時(shí)間: 2025-4-1 02:13
12C + 12C resonances studied in the elastic, inelastic, and transfer channels,esonances are characterized by large partial widths for decay into .C + .C, .C + .C(2.) and.C(2.). Assuming that .C + .C inelastic scattering data defines the gross features of the .Mg molecular spectrum, the possibility of directly exciting these states in the .C(.O,α) reaction at high energy is co
作者: BLANK 時(shí)間: 2025-4-1 09:14
Gross structure in mismatched channels,in inelastic channels which differ widely in their kinematic conditions from the elastic channel. Various models which explain the gross structure either as shape resonances or as diffractioe L window effects, are severely tested under these conditions. The symmetric .0 system offers a variety of si
作者: 闖入 時(shí)間: 2025-4-1 10:59
, ist t?glich mit der Aufgabe konfrontiert, Wissen aufzunehmen, anzupassen und zu verwenden. In Zeiten schneller ?nderungen am Markt, wachsender Bedürfnisse von Kunden und steigender Komplexit?t von Produkten ist es für Vertriebsmitarbeiter wichtig, durch ein effektives Wissensmanagement unterstützt
作者: fatty-streak 時(shí)間: 2025-4-1 14:44
Laminar Flow Control: Introduction and Overview,minar boundary layers can be stabilized by either favorable pressure gradients or small amounts of wall suction. (An excellent summary of this work is presented in References 1 and 2.) Research was performed in many countries to explore approaches for achieving extensive laminar flow with these conc
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