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Books on the topic 'Sea surface wave'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 November 2023

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1

Miller, James H. Estimation of sea surface wave spectra using acoustic tomography. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1987.

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2

Suoja, Nicole Marie. Directional wavenumber characteristics of short sea waves. Cambridge, Mass: Massachusetts Institute of Technology, 2000.

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3

V, Tatarskii Viatcheslav, and Environmental Technology Laboratory (Environmental Research Laboratories), eds. Phenomenological statistical non-Gaussian model of sea surface with anisotropic spectrum for wave-scattering theory. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1998.

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4

Jessup, Andrew T. Detection and characterization of deep water wave breaking using moderate incidence angle microwave backscatter from the sea surface. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1990.

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5

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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6

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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7

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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8

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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9

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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10

Environmental Technology Laboratory (Environmental Research Laboratories), ed. Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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11

R, Kerman B., and North Atlantic Treaty Organization. Scientific Affairs Division., eds. Sea surface sound: Natural mechanisms of surface generated noise in the ocean. Dordrecht: Kluwer Academic Publishers, 1988.

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12

Halpern, David. An atlas of monthly mean distributions of SSMI surface wind speed, AVHRR/2 sea surface temperature, AMI surface wind velocity, TOPEX/POSEIDON sea surface height, and ECMWF surface wind velocity during 1993. Pasadena, Calif: National Aeronautics and Space Administration, Jet Propulsion Laboratory, 1995.

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13

Halpern, D. An atlas of monthly mean distributions of SSMI surface wind speed, AVHRR/2 sea surface temperature, AMI surface wind velocity, TOPEX/POSEIDON sea surface height, and ECMWF surface wind velocity during 1993. Pasadena, Calif: National Aeronautics and Space Administration, Jet Propulsion Laboratory, 1995.

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14

Halpern, D. An atlas of monthly mean distributions of SSMI surface wind speed, AVHRR/2 sea surface temperature, AMI surface wind velocity, TOPEX/POSEIDON sea surface height, and ECMWF surface wind velocity during 1993. Pasadena, Calif: National Aeronautics and Space Administration, Jet Propulsion Laboratory, 1995.

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15

Halpern, D. An atlas of monthly mean distributions of SSMI surface wind speed, AVHRR/2 sea surface temperature, AMI surface wind velocity,and TOPEX/POSEIDON sea surface height during 1994. Pasadena, Calif: National Aeronautics and Space Administration, Jet Propulsion Laboratory, 1997.

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16

R, Kerman B., and Conference on Natural Physical Sources of Underwater Sound (1990 : Cambridge, England), eds. Natural physical sources of underwater sound: Sea surface sound (2). Dordrecht: Kluwer Academic Publishers, 1993.

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17

Kerman, B. R. Natural physical sources of underwater sound: Sea surface sound (2). Dordrecht: Springer Science, 1993.

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18

O'Muircheartaigh, I. G. Estimation of sea-surface windspeed from whitecap cover: Statistical approaches compared empirically and by simulation. Monterey, Calif: Naval Postgraduate School, 1985.

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19

1943-, Buckingham M. J., and Potter John, eds. Sea surface sound '94: Proceedings of the III International Meeting on Natural Physical Processes Related to Sea Surface Sound, University of California, Lake Arrowhead, 7-11 March 1994. Singapore: World Scientific, 1995.

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20

Lawrence, Richard T. Experimental inquires into collective sea state modes in deep water surface gravity waves. Monterey, Calif: Naval Postgraduate School, 1992.

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21

Egharevba, Frederick Efe. Ultrasonic surface waves seam tracking and penetration control in thin materials. Uxbridge: Brunel University, 1988.

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22

Laboratory, Wave Propagation, ed. Radar imaging of the sea surface using different polarizations: Comparison between theory and experiment. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Wave Propagation Laboratory, 1993.

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23

J, Gasiewski Albin, and United States. National Aeronautics and Space Administration., eds. Airborne passive polarimetric measurements of sea surface anisotropy at 92 GHz. [Washington, D.C: National Aeronautics and Space Administration, 1994.

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24

Principles of fluid flow and surface waves in rivers, estuaries, seas, and oceans. Amsterdam: Aqua Publications, 1990.

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25

1983-, Li Xiaofei, Diao Guijie 1982-, and Jiang Dan 1981-, eds. Shi bian hai mian lei da mu biao san she xian xiang xue mo xing: Radar phenomenological models for ships on time-evolving sea surface. Beijing Shi: Guo fang gong ye chu ban she, 2013.

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26

D, Vandemark, and Goddard Space Flight Center, eds. Airborne ROWS data report for the high resolution experiment. Greenbelt, Md: National Aeronautics and Space Administration, Goddard Space Flight Center, 1994.

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27

R, French Jeffrey, Crawford Timothy L, and Air Resources Laboratory (U.S.), eds. Aircraft measurements in the coupled boundary layers air-sea transfer (CBLAST) light wind pilot field study. Silver Spring, Md: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Oceanic and Atmospheric Research Laboratories, Air Resources Laboratory, 2001.

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28

Favre, A. Turbulent Fluxes Through the Sea Surface, Wave Dynamics, and Prediction. Springer, 2013.

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29

Favre, A. Turbulent Fluxes Through the Sea Surface, Wave Dynamics, and Prediction. Springer, 2011.

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30

Laser-glint measurements of sea-surface roughness. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Environmental Technology Laboratory, 1996.

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31

van der Hoeven, Frank, and Alexander Wandl. Hotterdam: How space is making Rotterdam warmer, how this affects the health of its inhabitants, and what can be done about it. TU Delft Open, 2015. http://dx.doi.org/10.47982/bookrxiv.1.

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Heat waves will occur in Rotterdam with greater frequency in the future. Those affected most will be the elderly – a group that is growing in size. In the light of the Paris heat wave of August 2003 and the one in Rotterdam in July 2006, mortality rates among the elderly in particular are likely to rise in the summer. METHOD The aim of the Hotterdam research project was to gain a better understanding of urban heat. The heat was measured and the surface energy balance modelled from that perspective. Social and physical features of the city we identified in detail with the help of satellite images, GIS and 3D models. We determined the links between urban heat/surface energy balance and the social/physical features of Rotterdam by multivariable regression analysis. The crucial elements of the heat problem were then clustered and illustrated on a social and a physical heat map. RESULTS The research project produced two heat maps, an atlas of underlying data and a set of adaptation measures which, when combined, will make the city of Rotterdam and its inhabitants more aware and less vulnerable to heat wave-related health effects. CONCLUSION In different ways, the pre-war districts of the city (North, South, and West) are warmer and more vulnerable to urban heat than are other areas of Rotterdam. The temperature readings that we carried out confirm these findings as far as outdoor temperatures are concerned. Indoor temperatures vary widely. Homes seem to have their particular dynamics, in which the house’s age plays a role. The above-average mortality of those aged 75 and over during the July 2006 heat wave in Rotterdam can be explained by a) the concentration of people in this age group, b) the age of the homes they live in, and c) the sum of sensible heat and ground heat flux. A diverse mix of impervious surfaces, surface water, foliage, building envelopes and shade make one area or district warmer than another. Adaptation measures are in the hands of residents, homeowners and the local council alike, and relate to changing behaviour, physical measures for homes, and urban design respectively.
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32

Kraus, Eric B., and Joost A. Businger. Atmosphere-Ocean Interaction. Oxford University Press, 1995. http://dx.doi.org/10.1093/oso/9780195066180.001.0001.

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With both the growing importance of integrating studies of air-sea interaction and the interest in the general problem of global warming, the appearance of the second edition of this popular text is especially welcome. Thoroughly updated and revised, the authors have retained the accessible, comprehensive expository style that distinguished the earlier edition. Topics include the state of matter near the interface, radiation, surface wind waves, turbulent transfer near the interface, the planetary boundary layer, atmospherically-forced perturbations in the oceans, and large-scale forcing by sea surface buoyancy fluxes. This book will be welcomed by students and professionals in meteorology, physical oceanography, physics and ocean engineering.
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33

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can have lifetimes varying from a few days to several weeks in the most extreme cases. Their presence can strongly affect the weather of large portions of the mid-latitudes, leading to the establishment of anomalous meteorological conditions. These can take the form of strong precipitation episodes or persistent anticyclonic regimes, leading in turn to floods, extreme cold spells, heat waves, or short-lived droughts. Even air quality can be strongly influenced by the establishment of atmospheric blocking, with episodes of high concentrations of low-level ozone in summer and of particulate matter and other air pollutants in winter, particularly in highly populated urban areas.Atmospheric blocking has the tendency to occur more often in winter and in certain longitudinal quadrants, notably the Euro-Atlantic and the Pacific sectors of the Northern Hemisphere. In the Southern Hemisphere, blocking episodes are generally less frequent, and the longitudinal localization is less pronounced than in the Northern Hemisphere.Blocking has aroused the interest of atmospheric scientists since the middle of the last century, with the pioneering observational works of Berggren, Bolin, Rossby, and Rex, and has become the subject of innumerable observational and theoretical studies. The purpose of such studies was originally to find a commonly accepted structural and phenomenological definition of atmospheric blocking. The investigations went on to study blocking climatology in terms of the geographical distribution of its frequency of occurrence and the associated seasonal and inter-annual variability. Well into the second half of the 20th century, a large number of theoretical dynamic works on blocking formation and maintenance started appearing in the literature. Such theoretical studies explored a wide range of possible dynamic mechanisms, including large-amplitude planetary-scale wave dynamics, including Rossby wave breaking, multiple equilibria circulation regimes, large-scale forcing of anticyclones by synoptic-scale eddies, finite-amplitude non-linear instability theory, and influence of sea surface temperature anomalies, to name but a few. However, to date no unique theoretical model of atmospheric blocking has been formulated that can account for all of its observational characteristics.When numerical, global short- and medium-range weather predictions started being produced operationally, and with the establishment, in the late 1970s and early 1980s, of the European Centre for Medium-Range Weather Forecasts, it quickly became of relevance to assess the capability of numerical models to predict blocking with the correct space-time characteristics (e.g., location, time of onset, life span, and decay). Early studies showed that models had difficulties in correctly representing blocking as well as in connection with their large systematic (mean) errors.Despite enormous improvements in the ability of numerical models to represent atmospheric dynamics, blocking remains a challenge for global weather prediction and climate simulation models. Such modeling deficiencies have negative consequences not only for our ability to represent the observed climate but also for the possibility of producing high-quality seasonal-to-decadal predictions. For such predictions, representing the correct space-time statistics of blocking occurrence is, especially for certain geographical areas, extremely important.
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34

Soloviev, Alexander, and Roger Lukas. The Near-Surface Layer of the Ocean. Springer, 2009.

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35

Askenazy, Philippe, and Bruno Palier. France. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198807032.003.0006.

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This chapter describes France as apparently one of the few rich countries to have avoided a significant increase in income inequality in recent decades. However, stable average inequalities mask an asymmetric trend of income between age groups, the elderly improving their situation while the young see theirs worsening. Furthermore, it shows that behind this relatively still surface, a general trend of precarization of more and more ordinary workers is occurring. The importance of wage-setting processes and of regulation of the labour market is brought out, together with the way the tax and transfer systems have operated, in restraining the forces driving inequality upwards. Wage growth, while limited, has thus been reasonably uniform across the distribution and together with the redistributive system have kept household income inequality within bounds. However, in response to high unemployment both regulatory and tax–transfer systems have served to underpin the very rapid growth in precarious working over the last decade, representing a very serious challenge for policy.
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36

Escudier, Marcel. Turbulent flow. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198719878.003.0018.

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In this chapter the principal characteristics of a turbulent flow are outlined and the way that Reynolds’ time-averaging procedure, applied to the Navier-Stokes equations, leads to a set of equations (RANS) similar to those governing laminar flow but including additional terms which arise from correlations between fluctuating velocity components and velocity-pressure correlations. The complex nature of turbulent motion has led to an empirical methodology based upon the RANS and turbulence-transport equations in which the correlations are modelled. An important aspect of turbulent flows is the wide range of scales involved. It is also shown that treating near-wall turbulent shear flow as a Couette flow leads to the Law of the Wall and the log law. The effect of surface roughness on both the velocity distribution and surface shear stress is discussed. It is shown that the distribution of mean velocity within a turbulent boundary layer can be represented by a linear combination of the near-wall log law and an outer-layer Law of the Wake.
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37

Soloviev, Alexander, and Roger Lukas. near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer, 2010.

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38

Soloviev, Alexander, and Roger Lukas. near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer, 2006.

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39

Soloviev, Alexander, and Roger Lukas. near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer London, Limited, 2013.

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40

Soloviev, Alexander, and Roger Lukas. The Near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer, 2013.

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41

Soloviev, Alexander, and Roger Lukas. The Near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer, 2013.

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42

Soloviev, Alexander, and Roger Lukas. The Near-Surface Layer of the Ocean: Structure, Dynamics and Applications. Springer, 2016.

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43

The Near-Surface Layer of the Ocean: Structure, Dynamics and Applications (Atmospheric and Oceanographic Sciences Library). Springer, 2006.

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