Ocean Tides Modeling Using Satellite Altimetry DISSERTATION
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OSTM/Jason-2 Products Handbook
OSTM/Jason-2 Products Handbook References: CNES : SALP-MU-M-OP-15815-CN EUMETSAT : EUM/OPS-JAS/MAN/08/0041 JPL: OSTM-29-1237 NOAA : Issue: 1 rev 0 Date: 17 June 2008 OSTM/Jason-2 Products Handbook Iss :1.0 - date : 17 June 2008 i.1 Chronology Issues: Issue: Date: Reason for change: 1rev0 June 17, 2008 Initial Issue People involved in this issue: Written by (*) : Date J.P. DUMONT CLS V. ROSMORDUC CLS N. PICOT CNES S. DESAI NASA/JPL H. BONEKAMP EUMETSAT J. FIGA EUMETSAT J. LILLIBRIDGE NOAA R. SHARROO ALTIMETRICS Index Sheet : Context: Keywords: Hyperlink: OSTM/Jason-2 Products Handbook Iss :1.0 - date : 17 June 2008 i.2 List of tables and figures List of tables: Table 1 : Differences between Auxiliary Data for O/I/GDR Products 1 Table 2 : Summary of error budget at the end of the verification phase 9 Table 3 : Main features of the OSTM/Jason-2 satellite 11 Table 4 : Mean classical orbit elements 16 Table 5 : Orbit auxiliary data 16 Table 6 : Equator Crossing Longitudes (in order of Pass Number) 18 Table 7 : Equator Crossing Longitudes (in order of Longitude) 19 Table 8 : Models and standards 21 Table 9 : CLS01 MSS model characteristics 22 Table 10 : CLS Rio 05 MDT model characteristics 23 Table 11 : Recommended editing criteria 26 Table 12 : Recommended filtering criteria 26 Table 13 : Recommended additional empirical tests 26 Table 14 : Main characteristics of (O)(I)GDR products 40 Table 15 - Dimensions used in the OSTM/Jason-2 data sets 42 Table 16 - netCDF variable type 42 Table 17 - Variable’s attributes 43 List of figures: Figure 1 -
Nitrogen Interception and Export by Experimental Salt Marsh Plots Exposed to Chronic Nutrient Addition
Vol. 400: 3–17, 2010 MARINE ECOLOGY PROGRESS SERIES Published February 11 doi: 10.3354/meps08460 Mar Ecol Prog Ser OPENPEN ACCESSCCESS FEATURE ARTICLE Nitrogen interception and export by experimental salt marsh plots exposed to chronic nutrient addition Lindsay D. Brin1, 2,*, Ivan Valiela2, Dale Goehringer3, Brian Howes3 1Brown University, Department of Ecology & Evolutionary Biology, 80 Waterman Street, Box G-W, Providence, Rhode Island 02912, USA 2The Ecosystems Center, Marine Biological Laboratory, 7 MBL St., Woods Hole, Massachusetts 02543, USA 3School of Marine Science and Technology, University of Massachusetts, Dartmouth, 706 South Rodney French Blvd., New Bedford, Massachusetts 02744, USA ABSTRACT: Mass balance studies conducted in the 1970s in Great Sippewissett Salt Marsh, New England, showed that fertilized plots intercepted 60 to 80% of the nitrogen (N) applied at several treatment levels every year from April to October, where interception mechanisms include plant uptake, denitrification and burial. These results pointed out that salt marshes are able to intercept land-derived N that could otherwise cause eutrophication in coastal waters. To determine the long-term N interception capacity of salt marshes and to assess the effect of different levels of N input, we measured nitrogenous materials in tidal water entering and leaving Great Sippewissett experimental plots in the 2007 growing season. Our results, from sampling over both full tidal cycles and more inten- sively sampled ebb tides, indicate high interception of Salt marshes limit the amount of land-derived nitrogen externally added N. Tidal export of dissolved inorganic carried by ebbing tides out to receiving coastal waters N (DIN) was small, although it increased with tide + Photo: Ivan Valiela height and at high N input rates. -
Ocean Surface Topography Altimetry by Large Baseline Cross-Interferometry from Satellite Formation
remote sensing Article Ocean Surface Topography Altimetry by Large Baseline Cross-Interferometry from Satellite Formation Weiya Kong 1,2, Bo Liu 2,*, Xiaohong Sui 2, Running Zhang 3 and Jinping Sun 1 1 School of Electronic and Information Engineering, Beihang University, Beijing 100191, China; [email protected] (W.K.); [email protected] (J.S.) 2 Qian Xuesen Laboratory of Space and Technology, Beijing 100094, China; [email protected] 3 Beijing Institute of Spacecraft System Engineering, Beijing 100094, China; [email protected] * Correspondence: [email protected]; Tel.: +86-010-6811-3401 Received: 21 September 2020; Accepted: 26 October 2020; Published: 27 October 2020 Abstract: Imaging Radar Altimeter (IRA) is the current development tendency for ocean surface topography (OST) altimetry,which utilizes Synthetic Aperture Radar (SAR) and interferometry to improve the spatial resolution of OST to several kilometers or even better. Meanwhile, centimetric altimetry accuracy should be guaranteed for applications such as geostrophic currents or marine gravity anomaly inversion. However, the baseline length of IRA which determines the altimetric sensitivity is confined by the satellite platform, in consideration of baseline vibration and payload capability. Therefore, the baseline length from a single satellite can extend to only tens of meters, making it difficult to achieve centimetric accuracy. Referring to the successful experience from TerraSAR-X/TanDEM-X, satellite formation can easily extend the baseline length to hundreds or thousands of meters, depending on the helix orbit. Therefore, we propose the large baseline IRA (LB-IRA) from satellite formation for OST altimetry: the carrier frequency shift (CFS) is brought in to compensate for the severe baseline decorrelation, and the helix orbit is carefully selected to prevent severe time decorrelation from along-track baseline. -
Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model
Washington State Department of Ecology Publication No. 12-03-049 PNNL-20384 Rev 1 Prepared for the U.S. Department of Energy under Contract DE-AC05-76RL01830 Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model by T Khangaonkar and W Long of the Pacific Northwest National Laboratory and B Sackmann, T Mohamedali, and M Roberts of the Washington State Department of Ecology November 2012 This page is purposely left blank This page is purposely left blank PNNL-20384 Rev 1 Puget Sound Dissolved Oxygen Modeling Study: Development of an Intermediate Scale Water Quality Model by T Khangaonkar and W Long of the Pacific Northwest National Laboratory B Sackmann, T Mohamedali, and M Roberts of the Washington State Department of Ecology October 2012 Prepared for the Washington State Department of Ecology under an Interagency Agreement with the U.S. Department of Energy Contract DE-AC05-76RL01830 Pacific Northwest National Laboratory Richland, Washington 99352 Any use of product or firm names in this publication is for descriptive purposes only and does not imply endorsement by the authors or the Department of Ecology. If you need this document in a format for the visually impaired, call 360-407-6764. Persons with hearing loss can call 711 for Washington Relay Service. Persons with a speech disability can call 877-833-6341. This page is purposely left blank Summary The Salish Sea, including Puget Sound, is a large estuarine system bounded by over seven thousand miles of complex shorelines, consists of several subbasins and many large inlets with distinct properties of their own. -
How a Tide Clock Works.Pub
Conventional time clocks have a 12 hour cycle, with 1 hand for hours, another for minutes. Tide clocks have a single hand, and a cycle of 12 hours 25 minutes, coinciding to an average time of about 6 hours 12 minutes between high and low tides. High tide is indicated when the hand is at the ‘12 o’clock’ position, low tide is indicated with the hand at the ‘6 o’clock’ position. A tide clock is not indicating 6 or 12 o’clock of course. It is merely a convenient reference point on the dial, showing us when our local tide is high or low. 12 is marked as High, 6 is marked as Low. However, the hour markings on the dial between the High and Low tide points do show us the number of hours since the last high or low tide, and the hours before the next high or low tide. A tide clock which has been initially set correctly will continue to display tide predictions quite accurately, requiring resetting only at intervals of about 4 months, depending upon the location. A brief explanation of how the tidal cycle works The Moon is the major cause of the tides. The ‘lunar day’ (the time it takes for the Moon to re-appear at the same place in the sky) is 24 hours and 50 minutes. New Zealand, and many other places in the world, have 2 high tides and 2 low tides each day. These are called semi-diurnal tides. Some areas of the world (eg Freemantle in Australia), have only one tide cycle per day, known as diurnal tides. -
Study of Earth's Gravity Tide and Ocean Loading
CHINESE JOURNAL OF GEOPHYSICS Vol.49, No.3, 2006, pp: 657∼670 STUDY OF EARTH’S GRAVITY TIDE AND OCEAN LOADING CHARACTERISTICS IN HONGKONG AREA SUN He-Ping1 HSU House1 CHEN Wu2 CHEN Xiao-Dong1 ZHOU Jiang-Cun1 LIU Ming1 GAO Shan2 1 Key Laboratory of Dynamical Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences, Wuhan 430077, China 2 Department of Land Surveying and Geoinformatics, Hong-Kong Polytechnic University, Hung Hom, Knowloon, Hong Kong Abstract The tidal gravity observation achievements obtained in Hongkong area are introduced, the first complete tidal gravity experimental model in this area is obtained. The ocean loading characteristics are studied systematically by using global and local ocean models as well as tidal gauge data, the suitability of global ocean models is also studied. The numerical results show that the ocean models in diurnal band are more stable than those in semidiurnal band, and the correction of the change in tidal height plays a significant role in determining accurately the phase lag of the tidal gravity. The gravity observation residuals and station background noise level are also investigated. The study fills the empty of the tidal gravity observation in Crustal Movement Observation Network of China and can provide the effective reference and service to ground surface and space geodesy. Key words Hongkong area, Tidal gravity, Experimental model, Ocean loading 1 INTRODUCTION The Earth’s gravity is a science studying the temporal and spatial distribution of the gravity field and its physical mechanism. Generally, its achievements can be used in many important domains such as space science, geophysics, geodesy, oceanography, and so on. -
Marine Pollution Bulletin 84 (2014) 191–200
Marine Pollution Bulletin 84 (2014) 191–200 Contents lists available at ScienceDirect Marine Pollution Bulletin journal homepage: www.elsevier.com/locate/marpolbul The effects of river run-off on water clarity across the central Great Barrier Reef ⇑ K.E. Fabricius a, , M. Logan a, S. Weeks b, J. Brodie c a Australian Institute of Marine Science, PMB No. 3, Townsville, Queensland 4810, Australia b Biophysical Oceanography Group, School of Geography, Planning and Environmental Management, University of Queensland, Brisbane 4072, Australia c Centre for Tropical Water & Aquatic Ecosystem Research, James Cook University, Townsville, Queensland 4811, Australia article info abstract Article history: Changes in water clarity across the shallow continental shelf of the central Great Barrier Reef were inves- Available online 23 May 2014 tigated from ten years of daily river load, oceanographic and MODIS-Aqua data. Mean photic depth (i.e., the depth of 10% of surface irradiance) was related to river loads after statistical removal of wave and Keywords: tidal effects. Across the 25,000 km2 area, photic depth was strongly related to river freshwater and Turbidity phosphorus loads (R2 = 0.65 and 0.51, respectively). In the six wetter years, photic depth was reduced Photic depth by 19.8% and below water quality guidelines for 156 days, compared to 9 days in the drier years. After Generalized additive mixed models onset of the seasonal river floods, photic depth was reduced for on average 6–8 months, gradually return- Great Barrier Reef ing to clearer baseline values. Relationships were strongest inshore and midshelf ( 12–80 km from the Nutrient runoff River floods coast), and weaker near the chronically turbid coast. -
Coupling of Repetitive Multibeam Surveys and Hydrodynamic Modelling to Understand Bedform Migration and Delta Evolution by Danar
Coupling of Repetitive Multibeam Surveys and Hydrodynamic Modelling to Understand Bedform Migration and Delta Evolution by Danar Guruh Pratomo B.Sc.Eng GGE, Institut Teknologi Bandung, 2003 M.Sc.Eng GGE, Institut Teknologi Bandung, 2007 A Dissertation Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in the Graduate Academic Unit of Geodesy and Geomatics Engineering Supervisor: John Hughes Clarke, Ph.D., Geodesy and Geomatics Engineering Examining Board: Susan Haigh, Ph.D., Fisheries and Oceans Canada Katy Haralampides, Ph.D., Civil Engineering Ian Church, Ph.D., University of Southern Mississippi External Examiner: Peter Talling, Ph.D., National Oceanography Course Southampton, UK This dissertation is accepted by the Dean of Graduate Studies THE UNIVERSITY OF NEW BRUNSWICK June, 2016 ©Danar Guruh Pratomo, 2016 ABSTRACT This study addresses channelized delta top sediment transport on the Squamish estuary in Howe Sound, British Columbia. The mechanism of bedform migration and delta evolution is affected by the manner in which the available sediment flux from the feeder fluvial system is distributed. The present study is complementary to a parallel project looking at the sediment migrating on the delta slope as landslides or turbidity currents. The termination of the Squamish River consists of a single channel that flows between flanking intertidal sand bars and over a mouth bar at the lip of the delta. The delta front is growing rapidly with about 1 million m3 of sediment being input from the river system annually. There is a 3 to 5 m tidal range that strongly modulates the flow in the channel and over the adjacent intertidal sand banks. -
Global Observations of Fine-Scale Ocean Surface Topography with the Surface Water and Ocean Topography (SWOT) Mission
fmars-06-00232 May 13, 2019 Time: 15:5 # 1 REVIEW published: 15 May 2019 doi: 10.3389/fmars.2019.00232 Global Observations of Fine-Scale Ocean Surface Topography With the Surface Water and Ocean Topography (SWOT) Mission Rosemary Morrow1*, Lee-Lueng Fu2, Fabrice Ardhuin3, Mounir Benkiran4, Bertrand Chapron3, Emmanuel Cosme5, Francesco d’Ovidio6, J. Thomas Farrar7, Sarah T. Gille8, Guillaume Lapeyre9, Pierre-Yves Le Traon4, Ananda Pascual10, Aurélien Ponte3, Bo Qiu11, Nicolas Rascle12, Clement Ubelmann13, Jinbo Wang2 and Edward D. Zaron14 1 Centre de Topographie des Océans et de l’Hydrosphère, Laboratoire d’Etudes en Géophysique et Océanographie Spatiale, CNRS, CNES, IRD, Université Toulouse III, Toulouse, France, 2 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States, 3 Laboratoire d’Océanographie Physique et Spatiale, Centre National de la Edited by: Recherche Scientifique – Ifremer, Plouzané, France, 4 Mercator Ocean, Ramonville-Saint-Agne, France, 5 Institut des Fei Chai, Géosciences de l’Environnement, Université Grenoble Alpes, Grenoble, France, 6 Sorbonne Université, CNRS, IRD, MNHN, Second Institute of Oceanography, Laboratoire d’Océanographie et du Climat: Expérimentations et Approches Numériques (LOCEAN-IPSL), Paris, France, State Oceanic Administration, China 7 Woods Hole Oceanographic Institution, Woods Hole, MA, United States, 8 Scripps Institution of Oceanography, University 9 Reviewed by: of California, San Diego, La Jolla, CA, United States, Laboratoire de Météorologie Dynamique (LMD-IPSL), -
Climate-Change–Driven Accelerated Sea-Level Rise Detected in the Altimeter Era
Climate-change–driven accelerated sea-level rise detected in the altimeter era R. S. Nerema,1, B. D. Beckleyb, J. T. Fasulloc, B. D. Hamlingtond, D. Mastersa, and G. T. Mitchume aColorado Center for Astrodynamics Research, Ann and H. J. Smead Aerospace Engineering Sciences, Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309; bStinger Ghaffarian Technologies Inc., NASA Goddard Space Flight Center, Greenbelt, MD 20771; cNational Center for Atmospheric Research, Boulder, CO 80305; dOld Dominion University, Norfolk, VA 23529; and eCollege of Marine Science, University of South Florida, St. Petersburg, FL 33701 Edited by Anny Cazenave, Centre National d’Etudes Spatiales, Toulouse, France, and approved January 9, 2018 (received for review October 2, 2017) Using a 25-y time series of precision satellite altimeter data from acceleration estimate by 0.033 mm/y2, resulting in a final “climate- TOPEX/Poseidon, Jason-1, Jason-2, and Jason-3, we estimate the change–driven” acceleration of 0.084 mm/y2. Climate-change–driven climate-change–driven acceleration of global mean sea level over in this case means we have tried to adjust the GMSL measurements the last 25 y to be 0.084 ± 0.025 mm/y2. Coupled with the average for as many natural interannual and decadal effects as we can to try climate-change–driven rate of sea level rise over these same 25 y of to isolate the longer-term, potentially anthropogenic, acceleration–– 2.9 mm/y, simple extrapolation of the quadratic implies global mean any remaining effects are considered in the error analysis. sea level could rise 65 ± 12 cm by 2100 compared with 2005, roughly We also must consider the impact of errors in the altimeter in agreement with the Intergovernmental Panel on Climate Change measurements, especially instrument drift. -
Title on the Observations of the Earth Tide by Means Of
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Kyoto University Research Information Repository On the Observations of the Earth Tide by Means of Title Extensometers in Horizontal Components Author(s) OZAWA, Izuo Bulletins - Disaster Prevention Research Institute, Kyoto Citation University (1961), 46: 1-15 Issue Date 1961-03-27 URL http://hdl.handle.net/2433/123706 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University DISASTER PREVENTION RESEARCH INSTITUTE BULLETIN NO. 46 MARCH, 1961 ON THE OBSERVATIONS OF THE EARTH TIDE BY MEANS OF EXTENSOMETERS IN HORIZONTAL COMPONENTS BY IZUO OZAWA KYOTO UNIVERSITY, KYOTO, JAPAN 1 DISASTER PREVENTION RESEARCH INSTITUTE KYOTO UNIVERSITY BULLETINS Bulletin No. 46 March, 1961 On the Observations of the Earth Tide by Means of Extensometers in Horizontal Components By Izuo OZAWA 2 On the Observations of the Earth Tide by Means of Extensometers in Horizontal Components By Izuo OZAWA Geophysical Institute, Faculty of Science, Kyoto University Abstract The author has performed the observations of tidal strains of the earth's surface in some or several directions by means of extensometers at Osakayama observatory Kishu mine, Suhara observatory and Matsushiro observatory, and he has calculated the tide-constituents (M2, 01, etc.) of the observed strains by means of harmonic analysis. According to the results, the phase lags of M2-constituents except one in Suhara are nearly zero, whose upper and lower limits are 43' and —29°, respectively. That is the coefficients of cos 2t-terms of the strains are posi- tive value in all the azimuths, and the ones of their sin 2t-terms are much smaller than the ones of their cos 2t-terms, where t is an hour angle of hypothetical heavenly body at the observatory. -
Earth Tide Effects on Geodetic Observations
EARTH TIDE EFFECTS ON GEODETIC OBSERVATIONS by K. BRETREGER A thesis submitted as a part requirement for the degree of Doctor of Philosophy, to the University of New South Wales. January 1978 School of Surveying Kensington, Sydney. This is to certify that this thesis has not been submitted for a higher degree to any other University or Institution. K. Bretreger ( i i i) ABSTRACT The Earth tide formulation is developed in the view of investigating ocean loading effects. The nature of the ocean tide load leads to a proposalfor a combination of quadratures methods and harmonic representation being used in the representation of the loading potential. This concept is developed and extended by the use of truncation functions as a means of representing the stress and deformation potentials, and the radial displacement in the case of both gravity and tilt observations. Tidal gravity measurements were recorded in Australia and Papua New Guinea between 1974 and 1977, and analysed at the International Centre for Earth Tides, Bruxelles. The observations were analysed for the effect of ocean loading on tidal gravity with a •dew to nodelling these effects as a function of space and time. It was found that present global ocean tide models cannot completely account for the observed Earth tide residuals in Australia. Results for a number of models are shown, using truncation function methods and the Longman-Farrell approach. Ocean tide loading effects were computed using a simplified model of the crustal response as an alternative to representation by the set of load deformation coefficients h~, k~. It is shown that a ten parameter representation of the crustal response is adequate for representing the deformation of the Earth tide by ocean loading at any site in Australia with a resolution of ±2 µgal provided extrapolation is not performed over distances greater than 10 3 km.