標(biāo)題: Titlebook: Air-Sea Exchange: Physics, Chemistry and Dynamics; G. L. Geernaert Book 1999 Springer Science+Business Media Dordrecht 1999 Coast.Ocean.at [打印本頁] 作者: 外表 時(shí)間: 2025-3-21 17:49
書目名稱Air-Sea Exchange: Physics, Chemistry and Dynamics影響因子(影響力)
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書目名稱Air-Sea Exchange: Physics, Chemistry and Dynamics讀者反饋學(xué)科排名
作者: 姑姑在炫耀 時(shí)間: 2025-3-21 22:23 作者: enlist 時(shí)間: 2025-3-22 02:20 作者: arbiter 時(shí)間: 2025-3-22 06:47
Effect of Surface Gravity Waves on Near-Surface Atmospheric Turbulence,nduced pressure component is far from satisfactory because very little is known about the structure of the wavw-induced flow in the atmospheric surface layer or how this flow affects the structure of the surface-layer turbulence.作者: Plaque 時(shí)間: 2025-3-22 11:22
Engineering Spectra Over Water,l on deep waters are sensitive to slow variation in the direction of the wind. Thus various engineering structures are sensitive to various components of wind fluctuations at a wide range of frequencies and also to the spatial correlations of these fluctuations.作者: cogent 時(shí)間: 2025-3-22 13:38 作者: insecticide 時(shí)間: 2025-3-22 17:55 作者: 昏迷狀態(tài) 時(shí)間: 2025-3-22 21:33 作者: 形容詞 時(shí)間: 2025-3-23 03:13 作者: canonical 時(shí)間: 2025-3-23 05:52 作者: 吞噬 時(shí)間: 2025-3-23 11:46
https://doi.org/10.1007/978-3-662-39795-4e distributions within the water column. In addition, biochemical processes acting on plantkonic matter, fungi, and bacteria, all exhibit an interplay with surface proceses (in particular in surface films), and this interplay governs air-sea exchange via both surface diffusion and wave breaking events.作者: 仔細(xì)檢查 時(shí)間: 2025-3-23 16:31
https://doi.org/10.1007/978-3-663-05290-6 complementary methods often are required to describe the turbulent atmosphere. The challenge for present-day observationalists is to choose the appropriate technology to fit a particular set of research needs — of course at a reasonable cost.作者: Between 時(shí)間: 2025-3-23 21:52 作者: 反復(fù)拉緊 時(shí)間: 2025-3-23 22:10
1383-8601 cts of the surface layer Monin-Obukhov (M-O) similarity theory for use over the sea, and to introduce and test new concepts related to high resolution flux magnitudes and variabilities. For example, data from various field experiments conducted on the North Sea, Lake Ontario, and the Atlantic experi作者: 慌張 時(shí)間: 2025-3-24 03:21
Das Verr?tselte: Emblematische Architektureffects. Over 40 year ago, to explain the radial increase in air temperature and specific humidity toward the center of tropical storms, Riehl (1954, p. 287) confidently stated that “A source for the heat and moisture increase is obvious. The ocean is greatly agitated, and large amounts of water are thrown into the air in the form of spray.”作者: 模范 時(shí)間: 2025-3-24 10:33
Das Verr?tselte: Emblematische Architekturia and production of hydrogen sulphide that these initiate, giving foul and smelling water, is promoted by deoxygenation (Tait 1981). The oxygen depletion is caused by an explosive growth of the biomass in the summer and the subsequent decay of this biomass is an oxygen consuming process.作者: Hormones 時(shí)間: 2025-3-24 14:05
Effekte des Grundmodells (Modellrechnung),portant concerns such as the fluxes of gases and nutrients and the growth and health of marine life. Improved understanding of all these processes depends in some measure on our understanding mechanisms and dynamics of the mixed layer.作者: fiscal 時(shí)間: 2025-3-24 15:45 作者: 豐滿中國 時(shí)間: 2025-3-24 19:42
Physical and Chemical Processes Governing Fluxes and Flux Divergence of Gaseous Ammonia and Nitric ia and production of hydrogen sulphide that these initiate, giving foul and smelling water, is promoted by deoxygenation (Tait 1981). The oxygen depletion is caused by an explosive growth of the biomass in the summer and the subsequent decay of this biomass is an oxygen consuming process.作者: GLOOM 時(shí)間: 2025-3-25 01:40 作者: 未完成 時(shí)間: 2025-3-25 03:36 作者: pantomime 時(shí)間: 2025-3-25 08:54 作者: 暫時(shí)休息 時(shí)間: 2025-3-25 13:23
https://doi.org/10.1007/978-3-662-39795-4hange. The atmospheric process which governs most air-sea exchanges is turbulent transport throughout the depth of the atmospheric boundary layer (ABL). The oceanic boundary layer influences many of the surface fluxes, via for example mixing associated with Langmuir circulations (LC’s) and the bubbl作者: LUT 時(shí)間: 2025-3-25 18:15
https://doi.org/10.1007/978-3-663-05290-6 atmosphere, and only in the last 70 years have those instruments been sensitive enough to measure turbulence. Now, we are probing atmospheric flows with sound, light, radio waves, and wires. Each of these media utilizes a different physical characteristic of air to measure different properties, and作者: insolence 時(shí)間: 2025-3-25 23:20
Das Atelier in der Fürstensuitehe wind, i.e. by wind waves, because these wave motions enhance transfer rates even when the surface is fairly smooth and continuous, and further enhance them when it breaks and forms sea spray. Thus, wind waves being the visual manifestation of the air-sea interaction, play an active role in this p作者: adequate-intake 時(shí)間: 2025-3-26 00:23
https://doi.org/10.1007/978-3-0346-0150-4gradually increase with fetch. Once developed, these wind waves play a significant role in the air-sea fluxes of momentum and energy, and modify the near surface atmospheric turbulence and the mean wind profile. This coupled system of wind and waves occurs over a wide variety of spatial and temporal作者: barium-study 時(shí)間: 2025-3-26 05:14 作者: 開始發(fā)作 時(shí)間: 2025-3-26 12:10
Das Verr?tselte: Emblematische Architekturthan the situation with a wind speed higher than the dominant wave speed. In view of obvious applications, the interest in situations with growing waves is natural. Nevertheless, as pointed out already by Kitaigorodskii (1973), possible widespread occurrence of ‘supersmooth flow’ (Donelan 1990) over作者: 跳動(dòng) 時(shí)間: 2025-3-26 12:39 作者: 終端 時(shí)間: 2025-3-26 17:38
https://doi.org/10.1007/978-3-0346-0150-4 adequately handling platform motion and maintaining measurement systems in harsh environments. However, we are approaching an era where, given the advancements in instrument technology and processing speed, these sorts of measurements are becoming increasingly routine. Through a number of past expe作者: Agnosia 時(shí)間: 2025-3-26 23:05 作者: dialect 時(shí)間: 2025-3-27 04:09 作者: 可以任性 時(shí)間: 2025-3-27 05:53 作者: Arthropathy 時(shí)間: 2025-3-27 10:21
Das Verr?tselte: Emblematische Architektur Over 50 years ago, Montgomery (1940) concluded that humidity profiles he collected over the ocean in winds less than 10 m/s showed evidence of spray effects. Over 40 year ago, to explain the radial increase in air temperature and specific humidity toward the center of tropical storms, Riehl (1954, 作者: Innocence 時(shí)間: 2025-3-27 16:35
https://doi.org/10.1007/978-3-0346-0150-4nition of the Beaufort wind scale. More recently, scientific curiosity about the contribution of sea spray to sea-air fluxes of heat and water vapour has led to significant progress in their quantification. Yet the fact that this is a difficult field and that there remain large gaps in our understan作者: NEXUS 時(shí)間: 2025-3-27 20:03
Das Verr?tselte: Emblematische Architekturon. This is a common problem in late summer, where the deoxygenation can lead to death of fish and benthic fauna. Furthermore growth of sulphur bacteria and production of hydrogen sulphide that these initiate, giving foul and smelling water, is promoted by deoxygenation (Tait 1981). The oxygen deple作者: 評(píng)論性 時(shí)間: 2025-3-28 00:02
https://doi.org/10.1007/978-3-0346-0150-4 loading on streamlines bridge decks requires knowledge of the vertical wind field fluctuations not only in one point, but also how the fluctuations are correlated in space (Simiu and Scanlan 1996; Larose, Mann 1998). Also the horizontal components may be of importance in bridge aerodynamics. For dy作者: 尖酸一點(diǎn) 時(shí)間: 2025-3-28 05:16
https://doi.org/10.1007/978-3-0346-0150-4nomena and to isolate their contribution to the evolving three-dimensional thermodynamic and kinematic fields. Because many MABL phenomena take the form of coherent structures in the turbulence field, much of this task becomes one of identifying and distinguishing the different coherent structure ty作者: 危險(xiǎn) 時(shí)間: 2025-3-28 07:34
Das Verr?tselte: Emblematische Architekturuxes of momentum, energy, and materials occur across the air-sea boundary. The boundary fluxes cause large normal (vertical) gradients in the adjacent velocity and buoyancy fields. The consequent shear and convective instabilities give rise to vigorous turbulence that carries the boundary fluxes som作者: medium 時(shí)間: 2025-3-28 10:28
Effekte des Grundmodells (Modellrechnung), oceanic surface mixed layer is the link by which the air and sea are coupled. Further, the form and strength of the mixing motion are important to important concerns such as the fluxes of gases and nutrients and the growth and health of marine life. Improved understanding of all these processes dep作者: 鑒賞家 時(shí)間: 2025-3-28 17:46 作者: 中世紀(jì) 時(shí)間: 2025-3-28 20:20 作者: Folklore 時(shí)間: 2025-3-29 02:25 作者: Matrimony 時(shí)間: 2025-3-29 03:23 作者: 一再困擾 時(shí)間: 2025-3-29 07:41
Book 1999re averaged for spatial footprints representing scales greater than 25 km (or typically 30 minutes or longer for typical windspeeds). While more and more data became available over the years, and the technology applied was more reliable, robust, and durable, the flux coefficients and other turbulent作者: disciplined 時(shí)間: 2025-3-29 12:21 作者: Sad570 時(shí)間: 2025-3-29 17:00 作者: 反抗者 時(shí)間: 2025-3-29 22:45
The Marine Atmospheric Boundary Layer During Swell, According to Recent Studies in the Baltic Sea,0-ies (Volkov 1970, Makova 1975; Benilov et al. 1974). Similar results were reported from measurements over Lake Michigan by Davidson and Frank (1973) and from waters outside the Australian coast by Antonia and Chambers (1980) and by Chambers and Antonia (1981).作者: DENT 時(shí)間: 2025-3-30 03:18
Flux Measurements at the Noordwijk Platform,ents. This has succesfully been done so far by Donelan et al. (1997) and Fairall et al. , (1997). In this way we can get a good approximation to the vertical wind, but what we need is w, the . vertical wind and the next problem is to find a place on board a ship where the flow is not severely distur作者: SEED 時(shí)間: 2025-3-30 05:16 作者: overwrought 時(shí)間: 2025-3-30 08:18
The Coastal Zone,ss and different surface heat flux over the sea. The modelling problem is particularly difficult with offshore flow of warm air over a cool water surface (Section 4). The development of stratus and other cloud regimes in the coastal zone is beyond the scope of this survey. This chapter will assume f作者: 不妥協(xié) 時(shí)間: 2025-3-30 14:39
Footprints of Atmospheric Phenomena in Synthetic Aperture Radar Images of the Ocean Surface: A Reviature on gravity capillary waves and also offers infrared images of their microscale breaking.) These waves can be an additional significant source of direct C-band radar backscatter for grazing angles between 60° and 10° (Plant 1997) as well as at smaller grazing angles (Smith et al. 1996). They ca作者: 變量 時(shí)間: 2025-3-30 19:54
The Droplets Produced by Individual Bubbles Bursting on a Sea Water Surface,nate single celled creatures have a hard time of it when exposed to a bubbling environment? Item: Some droplets created by bursting bubbles fly off at speeds of nearly 20 ms-1. Violent? Indeed. Complex and fascinating? Read on.作者: isotope 時(shí)間: 2025-3-30 21:32 作者: strain 時(shí)間: 2025-3-31 03:55 作者: FOLD 時(shí)間: 2025-3-31 07:15 作者: 品嘗你的人 時(shí)間: 2025-3-31 11:12 作者: Mammal 時(shí)間: 2025-3-31 15:41 作者: 修飾 時(shí)間: 2025-3-31 19:22 作者: 重力 時(shí)間: 2025-4-1 01:05 作者: Daily-Value 時(shí)間: 2025-4-1 05:21
https://doi.org/10.1007/978-3-0346-0150-4ss and different surface heat flux over the sea. The modelling problem is particularly difficult with offshore flow of warm air over a cool water surface (Section 4). The development of stratus and other cloud regimes in the coastal zone is beyond the scope of this survey. This chapter will assume f作者: 真 時(shí)間: 2025-4-1 06:10
Das Verr?tselte: Emblematische Architekturature on gravity capillary waves and also offers infrared images of their microscale breaking.) These waves can be an additional significant source of direct C-band radar backscatter for grazing angles between 60° and 10° (Plant 1997) as well as at smaller grazing angles (Smith et al. 1996). They ca作者: llibretto 時(shí)間: 2025-4-1 10:22 作者: faction 時(shí)間: 2025-4-1 15:42
https://doi.org/10.1007/978-3-0346-0150-4ithms cannot be developed for poorly understood or heretofore unknown structures. To reduce these problems, we develop a multi-pronged statistical approach that makes synergistic use of Principal COmponents Analysis, Fourier Spectral Analysis, and Fractal Dimension Analysis. Once identified by this 作者: BARK 時(shí)間: 2025-4-1 22:15
