Dissertations / Theses on the topic 'Wind speed at the sea surface'
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Avenas, Arthur. "Tropical cyclone dynamics revealed by satellite ocean surface wind speeds observations : the key contribution of the near-core surface wind structure." Electronic Thesis or Diss., Ecole nationale supérieure Mines-Télécom Atlantique Bretagne Pays de la Loire, 2024. http://www.theses.fr/2024IMTA0397.
Despite advances in predicting the tropical cyclones (TCs) trajectory and outer-core wind speeds, the numerical representation of the strongest winds associated with the most intense events is still an open issue, essentially because of the small radial extent of the TC core and the difficulty in understanding and resolving turbulent air-sea exchanges. Observational limitations have for a long time hindered accurate measurements of the ocean surface near the core region in extreme wind conditions, while geostationary satellites help characterizing the cloud patterns but lack direct information on the air-sea interface. Recently, synthetic aperture radar (SAR) has emerged as a promising satellite technology capable of producing high-resolution two dimensional measurements of the ocean surface wind speeds, thanks to new acquisition modes and algorithmic developments. Given these new observational opportunities, we investigate the contribution of near-core structural features, exclusively discernible through high-resolution instruments, to the TC dynamics. Using a simple theoretical framework and examining its consistency with SAR measurements, we demonstrate that the near-core surface winds modulate the evolution of the TC wind structure. The developed framework allows to illustrate how future measurements of ocean-atmosphere boundary layer characteristics could benefit the short- and long-term monitoring of TCs
Komarov, Alexander. "New methods for detecting dynamic and thermodynamic characteristics of sea ice from radar remote sensing." Institute of Electrical and Electronics Engineers, 2014. http://hdl.handle.net/1993/30225.
Zambra, Matteo. "Méthodes IA multimodales dans des contextes d’observation océanographique et de surveillance maritime multi-capteurs hétérogènes." Electronic Thesis or Diss., Ecole nationale supérieure Mines-Télécom Atlantique Bretagne Pays de la Loire, 2024. http://www.theses.fr/2024IMTA0391.
The aim of this thesis is to study the simultaneous use of heterogeneous ocean datasets to improve the performance of predictive models used in scientific and operational fields for the simulation and analysis of the ocean and marine environment. Two distinct case studies were explored in the course of the thesis work. The first study focuses on the local estimation of wind speed at the sea surface from underwater soundscape measurements and atmospheric model products. The second study considers the spatial extension of the problem and the use of observations at different scales and spatial resolutions, from pseudo-observations simulating satellite images to time series measured by in-situ infrastructures. The recurring theme of these investigations is the multi-modality of the data fed into the model. That is, to what extent and how the predictive model can benefit from the use of spatio-temporally heterogeneous information channels. The preferred methodological tool is a simulation system based on variational data assimilation and deep learning concepts
Song, Qingtao. "Surface wind response to oceanic fronts /." View online ; access limited to URI, 2006. http://0-wwwlib.umi.com.helin.uri.edu/dissertations/dlnow/3225330.
Sun, Yiping. "Sea state monitoring by radar altimeter from a microsatellite." Thesis, University of Surrey, 2001. http://epubs.surrey.ac.uk/844478/.
Park, Jeonghwan. "Investigations of GNSS-R for Ocean Wind, Sea Surface Height, and Land Surface Remote Sensing." The Ohio State University, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=osu1512095954817037.
Masson, Diane. "Spectral evolution of wind generated surface gravity waves in a dispersed ice field." Thesis, University of British Columbia, 1987. http://hdl.handle.net/2429/29020.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
Alamaro, Moshe 1948. "Wind wave tank for experimental investigation of momentum and enthalpy transfer from the ocean surface at high wind speed." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/51587.
Includes bibliographical references (leaves 77-79).
Thermodynamic analysis and numerical modeling of hurricane intensity has shown that its is controlled by the enthalpy transfer from the ocean surface and by drag. Direct measurements of drag, evaporation, and sensible heat transfer are not easily performed on the high seas. Therefore, a wind wave tank has been constructed in which a few aspects of a tropical storm are simulated. The air velocity inside the annular tank is comparable to that of hurricane. However, the three dimensionality of the tank obscures the quantitative comparison between experiments and actual conditions over the surface of the ocean at high wind speeds. The design of the wind wave tank and the initial experiments create a foundation for future and more comprehensive experimental programs. This thesis focuses mainly on the design and engineering of the tank, and on the fluid mechanics of the rotational flow in the tank. It also provides preliminary experimental data on the drag at high wind speeds obtained by using spindown experiments.
by Moshe Alamaro.
S.M.
Shinozuka, Yohei. "Sea-Salt Optical Properties Over the Remote Oceans: Their Vertical Profiles and Variations with Wind Speed." Thesis, University of Hawaii at Manoa, 2002. http://hdl.handle.net/10125/6961.
ix, 95 leaves
Mouton, Dawid Petrus. "Satellite derived sea surface temperature and wind field variability in the Benguela upwelling region." Master's thesis, University of Cape Town, 2002. http://hdl.handle.net/11427/6494.
Although upwelling was found to be more or less perennial along most of the coast south of 16 °S, seasonal variations were observed for both the SST and the upwelling favorable wind conditions. Inter-annual variability is common, and with these datasets it was possible to highlight periods of anomalous conditions. Results indicated that both the seasonal and inter-annual variability between the northern and southern parts of the Benguela system is quite different, with stronger seasonality observed in the southern Benguela.
Neeve, Michael Robert. "Easterly waves in the tropical Pacific." Thesis, University of Reading, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.362223.
EL-Nimri, Salem. "AN IMPROVED MICROWAVE RADIATIVE TRANSFER MODEL FOR OCEAN EMISSIVITY AT HURRICANE FORCE SURFACE WIND SPEED." Master's thesis, University of Central Florida, 2006. http://digital.library.ucf.edu/cdm/ref/collection/ETD/id/2523.
M.S.E.E.
School of Electrical Engineering and Computer Science
Engineering and Computer Science
Electrical Engineering
Ronglei, Hu, Yang Dongkai, Zhang Qishan, and Zhang Yiqiang. "DESIGN AND REALIZATION OF DELAY MAPPING RECEIVER BASED ON GPS FOR SEA SURFACE WIND MEASUREMENT." International Foundation for Telemetering, 2005. http://hdl.handle.net/10150/605046.
The Delay Mapping Receiver (DMR) is used for receiving and processing the reflected GPS signal to get the information of sea surface wind by recording and matching the data with the theoretical model. The hardware architecture and software design are described in detail in this paper. The test results at near sea of Tianjin of China are provided, which prove that the design of DMR is successful and the collected data are useful for the sea surface wind measurement.
Seymour, Sian. "Impact of Wind Driven Variability on Sea Surface Temperature and Ocean Colour in False Bay." Master's thesis, Faculty of Science, 2019. http://hdl.handle.net/11427/31235.
Zamo, Michaël. "Statistical Post-processing of Deterministic and Ensemble Wind Speed Forecasts on a Grid." Thesis, Université Paris-Saclay (ComUE), 2016. http://www.theses.fr/2016SACLA029/document.
Errors of numerical weather prediction (NWP) models can be reduced thanks to post-processing methods (model output statistics, MOS) that build a statistical relationship between the observations and associated forecasts. The objective of the present thesis is to build MOS for windspeed forecasts over France on the grid of several NWP models, to be applied on operations at Météo-France, while addressing the two main issues. First, building MOS on the grid of some NWP model, with thousands of grid points over France, requires to develop methods fast enough for operational delays. Second, requent updates of NWP models require updating MOS, but training MOS requires an NWP model unchanged for years, which is usually not possible.A new windspeed analysis for the 10 m windspeed has been built over the grid of Météo-France's local area, high resolution (2,5km) NWP model, AROME. The new analysis is the sum of two terms: a spline with AROME most recent forecast as input plus a correction with a spline with the location coordinates as input. The new analysis outperforms the existing analysis, while displaying realistic spatio-temporal patterns. This new analysis, now available at an hourly rate over 4, is used as a gridded observation to build MOS in the remaining of this thesis.MOS for windspeed over France have been built for ARPEGE, Météo-France's global NWP model. A test-bed designs random forests as the most efficient MOS. The loading times is reduced by a factor 10 by training random forests over block of nearby grid points and pruning them as much as possible. This time optimisation goes without reducing the forecast performances. This block MOS approach is currently being made operational.A preliminary study about the estimation of the continuous ranked probability score (CRPS) leads to recommendations to efficiently estimate it and to generalizations of existing theoretical results. Then 4 ensemble NWP models from the TIGGE database are post-processed with 6 methods and combined with the corresponding raw ensembles thanks to several statistical methods. The best combination method is based on the theory of prediction with expert advice, which ensures good forecast performances relatively to some reference forecast. This method quickly adapts its combination weighs, which constitutes an asset in case of performances changes of the combined forecasts. This part of the work highlighted contradictions between two criteria to select the best combination methods: the minimization of the CRPS and the flatness of the rank histogram according to the Jolliffe-Primo tests. It is proposed to choose a model by first imposing the flatness of the rank histogram
Da, Silva Meyre Pereira. "On the role of wind driven ocean dynamics in tropical Atlantic variability." Texas A&M University, 2003. http://hdl.handle.net/1969.1/3867.
Khattak, Sharafatullah. "Identification of sunglint areas in polar orbiting satellites imagery and determination of near-surface wind speed from sunglint radiance." Thesis, University of Dundee, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.340906.
Lamont, Tarron. "Comparative analysis of the seasonal sea surface temperature & wind stress in the four major eastern boundary current systems." Master's thesis, University of Cape Town, 2006. http://hdl.handle.net/11427/6486.
The coastal upwelling regions along northwest Africa (the Canary system), southwest Africa (the Benguela system), North America (the California system), and South America (the Peru-Chile system) were studied and compared on a seasonal timescale. A 17 -year NOAA Pathfinder Sea Surface Temperature (SST) dataset with a spatial resolution of 9km was used to describe the large-scale temporal and spatial variability of upwelling within the four regions. An upwelling index (OSST) was derived in order to add to the patterns of upwelling variability described from the sea surface temperature. The upwelling index was also used to describe the similarities and differences between the four upwelling regions. A 10-year ERS wind stress dataset with a spatial resolution of 10 x 10 was used to derive the offshore Ekman Transport in each of the regions. The offshore Ekman Transport was used to supplement the description of SST's in each system. Principal Component Analysis was used to investigate the variance structure of the anomalies of the sea surface temperature in each of the four regions. The results of the principal component analysis are interpreted in terms of the underlying physical dynamics.
Hesser, William A. "Global evaluation of special sensor microwave/imager ocean surface wind speed retrieval algorithms for the period September 1991 - April 1992." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1995. http://handle.dtic.mil/100.2/ADA303138.
Fang, Chin-Lung. "Predictability of Japan/East Sea (JES) system to uncertain initial/lateral boundary conditions and surface winds." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2003. http://library.nps.navy.mil/uhtbin/hyperion-image/03sep%5FFang.pdf.
Thesis advisor(s): Peter C. Chu, Steve Haeger. Includes bibliographical references (p. 73-77). Also available online.
Galea, Anthony. "Large-Eddy Simulation for wind and tidally driven sea circulation in coastal semi-closed areas." Doctoral thesis, Università degli studi di Trieste, 2014. http://hdl.handle.net/10077/10160.
A novel high-resolution, eddy-resolving numerical model (LES-COAST) is used to investigate currents, mixing and water renewal in Barcelona harbour and Taranto bay. These environmental sites are of particular importance due to the interplay between touristic and commercial activities, requiring detailed and high-definition studies of water quality within the harbour. We use Large Eddy Simulation (LES) which directly resolves the anisotropic and energetic large scales of motion and parametrizes the small, dissipative, ones. Small-scale turbulence is modelled by the Anisotropic Smagorinsky Model (ASM) which is employed in presence of large cell anisotropy. The complexity of the harbour is modelled using a combination of curvilinear, structured, non-staggered grid and the Immersed Boundary Method (IBM). Both computation grids and harbour structures are purposely constructed for these applications by appropriate programs. Boundary conditions for wind forcing at the free surface and currents at the inlets of the port are obtained from in-situ measurements (for the case of Barcelona harbour) or by nesting this numerical model into a coastal model (Taranto bay). In this dissertation thesis an important modification to LES-COAST is implemented and is proposed as a prototype scheme, namely the possibility to consider the effect of surface waves in coastal semi-closed areas. Particularly, a linear formulation of the free surface boundary condition is considered, which would be able to reproduce the presence of seiches and tides on the dynamics of the area under investigation. The methodology is validated against analytical solution for a stationary oscillating surface wave in a simple computational grid.In both harbours considered, first- and second-order statistics, such as the mean velocity field, turbulent kinetic energy, and horizontal and vertical eddy viscosities are calculated and their spatial distribution is assessed. Water residence time is also considered for the two coastal semi-closed areas examined. Finally, the LES solution is validated against available field data.The study shows the presence of sub-surface elongated rolling structures (with a time scale of a few hours), contributing to the vertical water mixing. The time-averaged velocity field reveals intense upwelling and downwelling zones along the walls of the harbours. The analysis of second-order statistics in these harbours shows strong inhomogeneity of turbulent kinetic energy and horizontal and vertical eddy viscosities in the horizontal plane, with larger values in the regions characterized by stronger currents. The water renewal within the port is quantified for particular sub-domain regions, showing that the complexity of the harbour is such that certain inner basins of Barcelona harbour have a water renewal of over five days, including its yacht marina area, and over seven days for Taranto bay. For the Barcelona simulation, the LES solution compares favourably with available current-meter data; it is also compared with a RANS solution obtained in literature for the same site under the same forcing conditions, the comparison demonstrating a large sensitivity of properties to model resolution and frictional parametrization.
XXVI Ciclo
1986
Du, Preez Chrisna Barbara. "A mesoscale investigation of the sea breeze in the Stellenbosch winegrowing district." Diss., Pretoria : [s.n.], 2007. http://upetd.up.ac.za/thesis/available/etd-02092007-093317.
Barrowes, Benjamin E. "YSCAT Backscatter Distributions." BYU ScholarsArchive, 2003. https://scholarsarchive.byu.edu/etd/67.
Maliniemi, V. (Ville). "Observations of solar wind related climate effects in the Northern Hemisphere winter." Doctoral thesis, University of Oulu, 2016. http://urn.fi/urn:isbn:9789526213545.
Anders, Ivonne [Verfasser], and Hans Von [Akademischer Betreuer] Storch. "Regional climate modelling : the Eastern European ”summer drying” problem and the representation of coastal surface wind speed in a multi model ensemble / Ivonne Anders. Betreuer: Hans von Storch." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2016. http://d-nb.info/1081768142/34.
Anders, Ivonne Verfasser], and Hans von [Akademischer Betreuer] [Storch. "Regional climate modelling : the Eastern European ”summer drying” problem and the representation of coastal surface wind speed in a multi model ensemble / Ivonne Anders. Betreuer: Hans von Storch." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2016. http://nbn-resolving.de/urn:nbn:de:gbv:18-77016.
Hung, Meng-Pai. "THE EVALUATION OF THE EAST GREENLAND SEA ODDEN ICE FEATURE USING THE COMMUNITY CLIMATE SYSTEM MODEL3.0 (CCSM3.0)." The Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=osu1250265410.
Samad-Suhaeb, Mujahid. "Aerodynamics of battle damaged finite aspect ratio wings." Thesis, Loughborough University, 2005. https://dspace.lboro.ac.uk/2134/10736.
Sasaki, Dalton Kei. "Mudanças dos Modos de Variabilidade do Atlântico Tropical no Século XX." Universidade de São Paulo, 2014. http://www.teses.usp.br/teses/disponiveis/21/21135/tde-10032015-151036/.
The results of SODA v2.2.6 reanalysis (Carton, Giese, 2008) and 20th Century Reanalysis v2 Project (Compo, et al., 2011) were analyzed in order to verify changes of the SST modes (the Meridional Temperature Gradient mode (GMT) and the Zonal Mode) in the Tropical Atlantic (1929 to 2008) using Empirical Orthogonal Functions (EOF) and joint Empirical Orthogonal Functions (jEOF). The spatial distribution of GMT starts initially as a temperature dipole centred at ≈ 5ºN. It evolves into a meridional gradient with variability concentrated at the Tropical North Atlantic. The zonal mode variability is initially associated with the equatorial region (between 5ºS and 5ºN) and with the northwestern african coast. It evolves into a merdional gradient with central axis located at 5ºN. Its variability is concentrated exclusively in the Tropical South Atlantic. The equatorial variability degenerates throughout the period, due to the inhibition of the isopicnal uplift by the wind. At the equator, the coupling occurs in periods of T = 30 months and T ≈ 34 months, with the wind preceding the TSM by 1 and 2 months, respectively. The zonal mode presents coupling with the wind only during the second half of the analysis. The periods are of T = 34 months, with wind preciding TSM by about 1 month. GMT mode is associated to the winds of both Tropical North Atlantic and Tropical South Atlantic. Coupling periods are of T = 96 and T = 60 months, with the wind preceding TSM in 3 and ≈ 2 months respectively.
Astudillo, Orlando. "Rôle des interactions océan-atmosphère-continent sur la dynamique de la couche limite marine dans la région d'upwelling du Chili central." Thesis, Toulouse 3, 2018. http://www.theses.fr/2018TOU30360.
Eastern Boundary Upwelling Systems (EBUS) are the tropical to mid-latitudes oceanic regions along the west coast of the continents. They host very productive marine ecosystems owing to the mean equatorward low-level atmospheric circulation that uplifts cool subsurface nutrient-enriched waters that trigger marine life along the coast. While the fundamental oceanic processes behind such process are well known (i.e. Ekman transport and pumping), the oceanic modeling of the EBUS has remained problematic owing to difficulties in accounting realistically for phenomena at fine spatial scales in the transition zone between the littoral and the off-shore ocean. In this thesis we have focused on the Peru-Chile Upwelling System (so-called Humboldt system) and on the influence of the cross-shore mesoscale features of the winds near the coast, particularly the shoreward wind drop-off, which determinate the relative importance of the Ekman processes, and thus, the spatial and temporal structure of the upwelling. A combined approach based on satellite data analysis and regional modeling, both oceanic and atmospheric, is used to investigate the sensitivity of the oceanic circulation along the coast of central Chile to the characteristics of the wind drop-off. As a first step, the mean to seasonal near-shore surface atmospheric circulation along the coast of Peru and Chile is documented for the first time based on the altimeter data from four satellite missions (ENVISAT, JASON1, JASON2 and SARAL). The analysis reveals the existence of a marked shoreward reduction in the wind speed all along the coast, although the reduction rate is latitudinally dependent. Despite the relatively weak repetitivity of the satellites, it is shown that the altimetric data are able to sample the seasonal cycle of the wind drop-off at some locations. The estimate of coastal upwelling from these data suggests that Ekman pumping tends on average to dominate with respect to Ekman transport over the Peruvian coast, whereas over the central-Chilean coast, the Ekman transport is the dominant process. In a second step, a regional atmospheric model (WRF) at different horizontal resolutions (36km, 12km and 4km) in a nested configuration zoomed over the central-Chile region was developed in order to produce atmospheric fields with different characteristics of the wind-stress curl (drop-off) along the coast. The atmospheric model solutions are first evaluated against the satellite observations, showing a much larger realism than atmospheric Reanalyses near the coast. In particular, the simulated cyclonic wind curl along the coast related to the wind drop-off exhibit length scales between 8 and 45 km with a significant latitudinal variability, which is in agreement with the altimetric winds. The higher model resolution, the more confined to the coast the wind drop-off, with the latter evidencing a marked seasonality with a maximum intensity in spring-fall and minimum in winter. The relative contribution of the coastal divergence and Ekman pumping exhibits a latitudinal modulation linked to details in the orography and coastlines
Villafañe, Roca Laura. "Experimental Aerothermal Performance of Turbofan Bypass Flow Heat Exchangers." Doctoral thesis, Universitat Politècnica de València, 2014. http://hdl.handle.net/10251/34774.
Villafañe Roca, L. (2013). Experimental Aerothermal Performance of Turbofan Bypass Flow Heat Exchangers [Tesis doctoral no publicada]. Universitat Politècnica de València. https://doi.org/10.4995/Thesis/10251/34774
TESIS
Xia, Yuan. "Sea-surface temperature and sea-surface wind-speed retrievals from spaceborne radiometer measurements." 2001. https://scholarworks.umass.edu/dissertations/AAI3012195.
Ko, Chih Shing, and 柯志軒. "Effects of wave height,wind speed on sea-surface wind stress." Thesis, 1994. http://ndltd.ncl.edu.tw/handle/38993908586679021907.
國立中山大學
海洋資源學系
82
A stable research platform,located at a coastal site off Taichung Harbor with an average water depth of about 8m,has been instrumented with a sonic anemometer with three-component wind speed, and air temperature sensors,and with three wind monitors at three different heights above the sea surface. A telemetry system has been used to transmit data to an inland receiving station.The wind turbulence data for the period between April 30 and November 19,1993 from this platform have been analyzed by the eddy correlation method to obtain wind stress and heat fluxes at various wind speeds. Data from near south-bound direction with longer fetch were used separately by the present study because it is unobstructed from the land and marine structures.Our results indicate that the wind stress is proportional to the square of wind speed.At lower winds,the drag coefficient,Cd,decteases with increaseing wind speed.At higher winds,it seems that Cd increases or remains unchanged with the wind speed.Cd was found to be generally larger for growing waves(smaller Co/u*)than for steady or decaying waves( larger Co/u*).The value of Cd with longer fetch from near north direction is generally higher than that with shorter fetch from near west direction.On the other hand,heat fluxes increase with the increasing wind speed and wave height.
Compton, Andrea Jean. "The correlation of sea surface temperatures, sea level pressure and vertical wind shear with ten tropical cyclones between 1981-2010." Thesis, 2013. http://hdl.handle.net/1805/3669.
Li, Hsien-Ming, and 李先明. "Seasonal and Interannual Variability of Satellite-derived Sea Surface Temperature and Sea Surface Wind in the Yellow Sea." Thesis, 2005. http://ndltd.ncl.edu.tw/handle/96665837872071639510.
國立臺灣海洋大學
海洋科學系
93
The purpose of this thesis is using satellite-derived sea surface temperature (SST) and sea surface wind data to investigate their variations in the Yellow Sea during the period from 1996 to 2003. The variation of the SST in the Yellow Sea is mainly seasonal. It is much lower and spatially non-homogeneous in winter than that in summer. A significant SST feature in winter is the Yellow Sea warm current, which is from the southwest side of Che-Ju Island. In summer, SST is warm except a cold water band distributed on the western Yellow Sea near the Korea Peninsula. The sea surface wind variation in the Yellow Sea is also seasonal. It is northerly in winter and southerly in summer. Wind speed in winter is higher than that in summer. In interannual scale, the highest SST anomaly temperature happened in June 1997, it seems to happen later than the onset of the El Niño. The wind speed shows lower value in 1997 and 1998 winter than the other years. The first SST empirical orthogonal function (EOF) mode, accounting for 98.2% of total variance, indicates again that low SST in winter and high SST in summer. The first spatial-demeaned EOF of SST, accounting for 78.3% in total variance, reveals mainly the sea surface circulation in winter. The first temporal-demeaned EOF of SST, containing 95.2% of total variance, shows clear SST variations in summer and winter, especially at coastal and deep water. Complex EOF mode 1 of SST reveals the SST patterns in the Yellow Sea mainly from southeast to northwest in summer. The first SST anomaly EOF, containing 43.7% of total variance, reveals a positive temperature anomaly during the 1997-1998 El Niño period. The wind speed and its anomaly EOFs show the variation of the monsoon patterns, which maybe affected by the influence of external factors (such as El Niño or atmospheric circulation). From the wind stress curl computation, it is suggested that the wind-induced anticyclonic sea surface circulation seems to be the reason to push the warm current into the Yellow Sea from south during the strong northerly monsoon season.
Huang, Shen-Cheng, and 黃舜成. "Determining sea surface wind from satellite microwave radiometric measurements." Thesis, 1996. http://ndltd.ncl.edu.tw/handle/73671883564683839979.
Chen, Ya-Wen, and 陳雅雯. "Satellite observations of the sea surface wind and temperature in the East China Sea." Thesis, 2004. http://ndltd.ncl.edu.tw/handle/75401767154404773761.
國立臺灣海洋大學
海洋科學系
92
Abstract In this study, the ERS-2 and QuikSCAT scatterometer and NOAA/AVHRR data from 1997 to 2001 are used to discuss the seasonal and inter-annual variations of the sea surface wind and sea surface temperature (SST) fields in the East China Sea (ECS). It is found that the sea surface wind and SST in the East China Sea are mainly annual. There is always a stronger northeastly in winter and weaker southly in summer. The results of the anomalous wind analysis indicate that the wind was behind the Southern Oscillation Index (SOI) about 4 months. Meanwhile, there is a weaker wind in 1997 fall/winter and 1998 spring. The SST in the ECS is colder in winter and warmer in summer and its spatial distribution is highly related to the bottom topography, especially in winter. The El Niño event in 1997 seems to cause a positive SST anomaly during December 1997 to November 1998. Keywords: East China Sea, satellite sea surface wind, satellite sea surface temperature, El Niño event.
Yang, Hong-Yuan, and 楊弘源. "Satellite observations of chlorophyll-a concentration and sea surface wind in the South China Sea." Thesis, 2005. http://ndltd.ncl.edu.tw/handle/49267887105157509242.
國立臺灣海洋大學
海洋科學系
93
The purpose of this thesis is using Orbview-2/Sea-viewing Wide Field-of-view Sensor (SeaWiFS), and European Remote Sensing Satellite (ERS) -1/2 and Quick Scatterometer (QuikSCAT)/SeaWinds satellite data to discuss the chlorophyll-a (Chl-a) concentration and sea surface wind fields in the South China Sea (SCS). Chl-a in the SCS is nearly annual. Mode 1 results of the Chl-a empirical orthogonal function (EOF) analysis indicate that the higher Chl-a is mainly along the coastal areas, while the much lower Chl-a is in the offshore areas. EOF mode 2 results show a summer-winter oscillation of the Chl-a distribution in the SCS. The Chl-a anomaly data can be used to see its interannual variation. Through the comparison between EOF mode 2 results of the Chl-a anomaly and Niño 3.4 index, we find that Chl-a in the SCS is highly related to the ENSO events. The wind speed in the SCS is also annual. There is a northeasterly monsoon in winter, and a southwesterly monsoon in summer. Wind speed EOF mode 1 results indicate that the northeasterly monsoon is much stronger than southwesterly monsoon. The EOF mode 2 results of the sea surface wind indicate that the zonal area near 15。N can be a boundary to separate the wind pattern into two parts during fall, the wind in the north part is northeasterly and southwesterly in the south. Comparing Chl-a EOF mode 2 and wind speed EOF mode 1 results, we can find that Chl-a in the SCS is mainly influenced by the monsoon wind. Wind-induced coastal upwelling makes the Chl-a increase along the western SCS in summer and the eastern SCS in winter.
Anderson, SallyRose. "Wind River Range Snowpack Reconstruction Using Dendochronology and Sea Surface Temperatures." 2010. http://trace.tennessee.edu/utk_gradthes/771.
Chen-YuChen and 陳振宇. "Effects of Wind Speed and Temperatures on the Radar Sea Return at X-band." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/52112847718926680609.
國立成功大學
水利及海洋工程學系碩博士班
101
Since Mattie and Harris (1978) used different frequency bands of radar for observing the waves, the X-Band microwave radar has been applied for observing the sea waves. In recent years, the X-band microwave radar applications are becoming more common on the ocean observing. We can analyze the characteristics of the sea waves indirectly by the radar sea return signals. Sea and Meteorology parameters such as air temperature, water temperature, wind speed, etc. affect the sea surface roughness and the X-Band microwave radar observations. This study explores the X-band microwave radar sea return with weather stations and buoys data collected at Xingda Harbour sea area. The data analysis is divided into two parts: The first part compares the relationship between wind speed and radar sea return in the same air temperature. The other part compares the relationship between radar sea return and the difference between air and sea temperatures in the same wind speed. In addition, there are unusual radar sea return signals on the radar image nearby the place of the wastewater emissions. And the study explores the X-band microwave radar sea return with water temperature, the difference between air and sea temperatures, and the surface tension by using measured water temperature, the surface tension of CRC Handbook of Chemistry and Physics and the air temperature of weather stations.
Yu, Yunyue. "Sea surface temperature, geostrophic current and surface heat advection in the western tropical Pacific." 1996. http://catalog.hathitrust.org/api/volumes/oclc/37356621.html.
"Impact of Grid Resolution on Atmospheric Model Simulation of Offshore Surface Wind Speed." Master's thesis, 2012. http://hdl.handle.net/2286/R.I.15026.
Dissertation/Thesis
M.S. Mechanical Engineering 2012
Lai, You-Cheng, and 賴佑晟. "Investigation of the Sea Surface Wind and Flux for the Development of Tropical Cyclone." Thesis, 2017. http://ndltd.ncl.edu.tw/handle/jhkw3r.
國立中央大學
大氣科學學系
105
The genesis and intensification of tropical cyclone(TC) are usually occurring in the ocean where is lacking those traditional observations like surface in-situ data or radiosounde for upper atmosphere. Therefore, satellite data plays a critical role in the purpose of simulation and/or forecast of TC in these stages, and the further investigation of the evolution and intensity intensification. According to the earlier studies, part of the energy for TC intensification is associated with the planetary boundary processes, which might be through the air-sea interaction like latent heat flux and sensible heat flux. Furthermore, sea surface wind could be an important role between sea and air when gradient is presented. Therefore, sea surface wind data from the Advanced Scatterometer (ASCAT) which is aboard on ESA Metop-A satellite are used to address this issue in this study through the data assimilation technique and the use of regional Weather Research and Forecasting (WRF) model. The main focus is placed on the investigation of the impacts from sea surface wind, sensible heat flux, and latent heat flux for the TC forecast. The discussion on the relative importance of those above fluxes during the TC intensification stage. This study is divided into two parts: data assimilation experiment and sensitivity experiment. Typhoon Nuri (2008) in the northwestern Pacific Ocean is chosen to elaborate those fluxes and roles as described. In first part of experiment, the best forecast skill is from the use of ASCAT and traditional observation data sets, by examination of the TC’s intensity and track forecasts. This is due to the ASCAT data can improve the structure of surface wind in the initial time. In second part, the sensitivity experiment, we find the higher sea surface temperature might increase the temperature gradient between the sea and the air. It leads an increased air-sea flux and a stronger TC in the later forecast hours. It is also found that the sea surface wind plays an important role in the sea-air flux, that is, if there is a large temperature or humidity gradient between sea and air, the energy conversion efficiency will be poor due to the weak sea surface wind speed. Thus, TC obtains less energy from the ocean and the intensity will not be intensified. Cross-analysis of the above simulations, we conclude that the larger fluxes in the early stage of the Typhoon Nuri, the more energy can be obtained from the ocean and the intensity will become stronger.
Lai, Fei, and 賴飛. "A Study on Wind-Induced Sea Surface Roughness in the Eest of Hengchun Peninsula." Thesis, 2017. http://ndltd.ncl.edu.tw/handle/8aqwhw.
國立臺灣海洋大學
海洋環境資訊系
105
Is this study, the relationship between wind-induced sea surface roughness (SSR) and sea surface temperature (SST) in the west of Hengchun Peninsula is investigated using satellite Synthetic Aperture Radar (SAR) and thermal infrared data. The normalized radar cross section (NRCS) derived from SAR data can represent the wind speed, because wind speed is related to SSR. After comparing with these two data, a negative linear relationship is found between NRCS and SST. Higher NRCS, that is, higher SSR has lower SST. The gradient of the linear relationship is then compared with the difference between air temperature and SST. The result shows a very good correlation at the condition of SST is higher than air temperature. This indicates that the higher temperature difference between air and sea can increase the release of heat from the ocean to the atmosphere.
Sušelj, Kay [Verfasser]. "Modelling of the near-surface wind speed : boundary layer and climate aspects / von Kay Sušelj." 2009. http://d-nb.info/996766146/34.
Mahajan, Salil. "Free and forced tropical variability: role of the wind-evaporation-sea surface temperature (WES) feedback." Thesis, 2008. http://hdl.handle.net/1969.1/ETD-TAMU-3107.
Hsieh, Yu-Chi, and 謝玉琪. "Satellite Observation of Sea Surface Temperature, Chlorophyll-a Concentration and Wind of the Luzon Strait." Thesis, 2007. http://ndltd.ncl.edu.tw/handle/22295153248369165711.
國立臺灣海洋大學
海洋環境資訊學系
95
Abstract The purpose of this thesis is to discuss the variation of the Aqua satellite Moderate-resolution Imaging Spectroradiometer (MODIS) sea surface temperature (SST) and chlorophyll-a (Chl-a) data in the Luzon Strait during the period between 2002 and 2006 and the related Quick Scatterometer (QuikSCAT) satellite SeaWinds data from 1999 to 2006. From SST satellite images, it is found that the Kuroshio intrusion into the Luzon Strait is much clearer in winter than in summer. Meanwhile, the stronger sea surface wind can push the Kuroshio more westerward during wintertime. From Chl-a satellite images, the intrusion of the low Chl-a Kuroshio is much more obvious than that in SST images, it always displays as a clockwise loop to intrude the Luzon Strait. Comparing SST with Chl-a data, we can see a negative correlation between them in the study area, especially in the west of the Kuroshio. In interannual scale, the summer 2004 and summer 2006 are the coldest and warmest summer, respectively. Besides, the wind speed shows a clear decreasing trend during 1999~2002 no matter in summer or winter.
Chen, Chien-Ming, and 陳建銘. "Wind and Diurnal Effect on the Accuracy of Sea Surface Temperature Measurements from Geostationary Satellite." Thesis, 2004. http://ndltd.ncl.edu.tw/handle/28692945954743841040.
LEE, WEN HORNG, and 李文鴻. "Estimation of wind stress and heat flux over the sea surface by the inertial-dissiption method." Thesis, 1995. http://ndltd.ncl.edu.tw/handle/57902233521198500058.
國立中山大學
海洋資源學系
83
Measurements of instantaneous wind speed and air temperature at nearly 10m above the mean sea surface as well as the sea- surface temperature were made during three cruises of R/V Ocean Researcher Ⅲ over southern Taiwna Strait. Inertial- dissipation method was used to estimate the wind stree and sensible heat flux. From spectra of wind speed and temperature it is clearly shown that the inertial subrange typically exists in high frequency band (0.5Hz-10Hz) and the -5/3 power law applies in this region. The downwind spectral value φu was found to be 3/4 times φv, the cross wind spectral value,i.e. the conditon of isotropy was satisfied. The wind spectral increases with the third power of the wind speed, and spectral value of temperature correlates well with U10n(Ts-θa), where U10n is the wind speed at 10m height under neutral condition, Ts and θa are the sea-surface and air potential temperatures respectively. Effects of atmospheric stability on momentum fluxes are especially significant under conditions of low wind and large air-sea temperature difference. Our results indicate that wind stress increase with the 7/3 power of wind speed. Neutral drag coefficent CD10n increses with increasing wind speed. Sensible heat flux has a linear relationship with U10(Ts- θa). Heat flux coefficent CT10n remains constant with varying atmospheric stability parameters under unstable stratifictions. These results are consistent wind previous studies. Finally, a time-series comparison was also made between wind stress derived from dissipation and bulk methods. Our results show that dissipation estimates of the wind stress agree well with those from bulk method and the differences are generally less than 20 percents.
Cheng, Wan-Chen, and 鄭婉貞. "Impacts of two-type El Niño/La Niña on Sea Surface Wind over the Tropical Pacific." Thesis, 2013. http://ndltd.ncl.edu.tw/handle/77nsg2.
國立臺灣海洋大學
海洋環境資訊學系
101
In this study, different index values are used to select months of El Niño, El Niño Modoki, La Niña and La Niña Modoki, respectively. This case selection method (also called Niño Matrix Method) is applied to NCEP/NCAR reanalysis data to investigate the impacts of two-type El Niño/La Niña on sea surface wind over the tropical Pacific druing years of 1950~2011. The results show that the impacts of both types of El Niño/La Niña on sea surface wind over the tropical Pacific are different. Westerly anomalies of wind speed appear in the equatorial Pacific during both types of El Niño, while the values of El Niño Modoki are stronger than those of El Niño. The location with maximum value of westerly anomalies of El Niño Modoki is far west of that of El Niño. In the western Pacific near land, easterly anomalies of El Niño Modoki are also larger than those of El Niño. As for La Niña, easterly anomalies of wind speed appeare in the equatorial Pacific during both types of La Niña. The values of La Niña Modoki are stronger than those of La Niña. The range of easterly anomalies of La Niña Modoki is smaller than that of La Niña. During the period of La Niña Modoki, westerly anomalies also appear in the eastern Pacific.