Relevant bibliographies by topics / Storm morphology

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Storm morphology'

Author: Grafiati
Published: 4 June 2021
Last updated: 8 February 2022

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Journal articles on the topic "Storm morphology"

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Stein, Thorwald H. M., Robin J. Hogan, Kirsty E. Hanley, et al. "The Three-Dimensional Morphology of Simulated and Observed Convective Storms over Southern England." Monthly Weather Review 142, no. 9 (2014): 3264–83. http://dx.doi.org/10.1175/mwr-d-13-00372.1.

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A set of high-resolution radar observations of convective storms has been collected to evaluate such storms in the Met Office Unified Model during the Dynamical and Microphysical Evolution of Convective Storms (DYMECS) project. The 3-GHz Chilbolton Advanced Meteorological Radar was set up with a scan-scheduling algorithm to automatically track convective storms identified in real time from the operational rainfall radar network. More than 1000 storm observations gathered over 15 days in 2011 and 2012 are used to evaluate the model under various synoptic conditions supporting convection. In ter
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Marmoush, Ramy Y., and Ryan P. Mulligan. "OBSERVATIONS OF BEACH-DUNE MORPHOGOLICAL RESPONSE TO STORM WAVES USING LIDAR BATHYMETRIC MAPPING IN A WAVE BASIN." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 5. http://dx.doi.org/10.9753/icce.v36.sediment.5.

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Waves during major storms can cause significant changes to coastal morphology (Lee et al., 1998). The beach-dune system is known to be highly vulnerable to erosion when the wave run-up exceeds the threshold of the base of the dune in the collision regime, according to the Storm Impact scale defined by Sallenger (2000). Detailed bathymetric measurements are very difficult to obtain during storms due to the hazardous wave conditions. However, bathymetric surveys can be easily and intermittently performed during smaller scale physical model experiments (e.g., Hamilton et al., 2001) and high resol
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Markowski, Paul, and Yvette Richardson. "On the Classification of Vertical Wind Shear as Directional Shear versus Speed Shear." Weather and Forecasting 21, no. 2 (2006): 242–47. http://dx.doi.org/10.1175/waf897.1.

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Abstract Vertical wind shear is commonly classified as “directional” or “speed” shear. In this note, these classifications are reviewed and their relevance discussed with respect to the dynamics of convective storms. In the absence of surface drag, storm morphology and evolution only depend on the shape and length of a hodograph, on which the storm-relative winds depend; that is, storm characteristics are independent of the translation and rotation of a hodograph. Therefore, traditional definitions of directional and speed shear are most relevant when applied to the storm-relative wind profile
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Li, Honghai, Lihwa Lin, and Kelly A. Burks-Copes. "NUMERICAL MODELING OF COASTAL INUNDATION AND SEDIMENTATION BY STORM SURGE, TIDES, AND WAVES AT NORFOLK, VIRGINIA, USA." Coastal Engineering Proceedings 1, no. 33 (2012): 54. http://dx.doi.org/10.9753/icce.v33.sediment.54.

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A nearshore hydrodynamic and sediment transport model was developed to simulate synthetic storms with design SLR scenarios surrounding the military installations in Norfolk, Virginia. Foreseeable risk and effect of storm surge damage accompanied by waves, tides, and Sea Level Rise (SLR) were examined. The final results include the evaluation of impacts for five SLR (0.0, 0.5, 1.0, 1.5, and 2.0 m) and three storm conditions (50-yr, 100-yr return tropical storms, and a winter storm). Associated with the storm surge and SLR, extensive inundation will occur at the Naval Station Norfolk, approximat
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Burns, A. G., T. L. Killeen, and R. G. Roble. "Thermospheric heating away from the auroral oval during geomagnetic storms." Canadian Journal of Physics 70, no. 7 (1992): 544–52. http://dx.doi.org/10.1139/p92-089.

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Model predictions indicate that the high-latitude thermosphere near the F2 peak undergoes strong heating during geomagnetic storms. Experimental studies at middle and equatorial latitudes have indicated that heating occurs during geomagnetic storms, although the overall morphology of these temperature changes is not clear. In this paper we use data from the DE-2 (dynamics explorer) satellite to study this morphology at middle and high latitudes, and then use a simulation of the November 24, 1982 storm, by the NCAR–TIGCM, to compare model output and data on a "one-on-one" basis for an individua
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Palermo, Rose V., Anastasia Piliouras, Travis E. Swanson, Andrew D. Ashton, and David Mohrig. "The effects of storms and a transient sandy veneer on the interannual planform evolution of a low-relief coastal cliff and shore platform at Sargent Beach, Texas, USA." Earth Surface Dynamics 9, no. 5 (2021): 1111–23. http://dx.doi.org/10.5194/esurf-9-1111-2021.

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Abstract. Coastal cliff erosion is alongshore-variable and episodic, with retreat rates that depend upon sediment as either tools of abrasion or protective cover. However, the feedbacks between coastal cliff planform morphology, retreat rate, and sediment cover are poorly quantified. This study investigates Sargent Beach, Texas, USA, at the annual to interannual scale to explore (1) the relationship between temporal and spatial variability in cliff retreat rate, roughness, and sinuosity and (2) the response of retreat rate and roughness to changes in sand and shell hash cover of the underlying
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Mendillo, M., and C. Narvaez. "Ionospheric storms at geophysically-equivalent sites – Part 1: Storm-time patterns for sub-auroral ionospheres." Annales Geophysicae 27, no. 4 (2009): 1679–94. http://dx.doi.org/10.5194/angeo-27-1679-2009.

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Abstract. The systematic study of ionospheric storms has been conducted primarily with groundbased data from the Northern Hemisphere. Significant progress has been made in defining typical morphology patterns at all latitudes; mechanisms have been identified and tested via modeling. At higher mid-latitudes (sites that are typically sub-auroral during non-storm conditions), the processes that change significantly during storms can be of comparable magnitudes, but with different time constants. These include ionospheric plasma dynamics from the penetration of magnetospheric electric fields, enha
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Ellis, Jean T., Michelle E. Harris, Mayra A. Román-Rivera, J. Brianna Ferguson, Peter A. Tereszkiewicz, and Sean P. McGill. "Application of the Saffir-Simpson Hurricane Wind Scale to Assess Sand Dune Response to Tropical Storms." Journal of Marine Science and Engineering 8, no. 9 (2020): 670. http://dx.doi.org/10.3390/jmse8090670.

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Over one-third of the Earth’s population resides or works within 200 km of the coast. The increasing threat of coastal hazards with predicted climate change will impact many global citizens. Coastal dune systems serve as a natural first line of defense against rising sea levels and coastal storms. This study investigated the volumetric changes of two dune systems on Isle of Palms, South Carolina, USA prior to and following Hurricanes Irma (2017) and Florence (2018), which impacted the island as tropical storms with different characteristics. Irma had relatively high significant wave heights an
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Mickey, Rangley C., Patricia S. Dalyander, Robert McCall, and Davina L. Passeri. "Sensitivity of Storm Response to Antecedent Topography in the XBeach Model." Journal of Marine Science and Engineering 8, no. 10 (2020): 829. http://dx.doi.org/10.3390/jmse8100829.

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Antecedent topography is an important aspect of coastal morphology when studying and forecasting coastal change hazards. The uncertainty in morphologic response of storm-impact models and their use in short-term hazard forecasting and decadal forecasting is important to account for when considering a coupled model framework. This study provided a methodology to investigate uncertainty of profile response within the storm impact model XBeach related to varying antecedent topographies. A parameterized island Gaussian fit (PIGF) model generated an idealized baseline profile and a suite of idealiz
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Lucrezi, Serena, Thomas A. Schlacher, and Wayne Robinson. "Can storms and shore armouring exert additive effectson sandy-beach habitats and biota?" Marine and Freshwater Research 61, no. 9 (2010): 951. http://dx.doi.org/10.1071/mf09259.

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Increased storminess is a likely consequence of global climate change; its effects may be most dramatic on coasts dominated by sandy beaches. This scenario demands that the impacts of storms and the role of armouring structures, constructed as storm defences, are better understood. Here, we assess how a relatively small storm affected beach morphology and macrobenthos, and whether a seawall can modulate such impacts. The study system was a small (<1.5 km long) beach, bisected into parts with and without a seawall. The beach became narrower and steeper during the storm, when 26% of the subae
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Dissertations / Theses on the topic "Storm morphology"

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Thomas, Evan Grier. "Morphology and dynamics of storm-time ionospheric density structures." Diss., Virginia Tech, 2016. http://hdl.handle.net/10919/64905.

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Accurate knowledge of the electron density structure of the Earth's upper atmosphere is crucial to forecasting the performance of transionospheric radio signals. For this research, we focus on storm-time structuring in the mid- to high latitude ionosphere where large gradients in electron density can cause severe degradation of communication and navigation signals. We begin in Chapter 2 with a review of the primary data sets and methods used to accomplish the collaborative, multi-instrument studies described in this dissertation. In Chapter 3, we compare observational techniques for trackin
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McCall, Robert Timothy. "Process-based modelling of storm impacts on gravel coasts." Thesis, University of Plymouth, 2015. http://hdl.handle.net/10026.1/3929.

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Gravel beaches and barriers occur on many high-latitude, wave-dominated coasts across the world. Due to their natural ability to dissipate large amounts of wave energy, gravel coasts are widely regarded as an effective and sustainable form of coastal defence. However, during extreme events waves may overtop, overwash, and even lower, the crest of the gravel beach, flooding the hinterland. In the evaluation of the safety of gravel coasts against flooding, coastal managers currently rely on models that have been shown in previous studies to be inaccurate. The research in this thesis attempts to
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Gartner, Joseph E. "Relations between wildfire related debris-flow volumes and basin morphology, burn severity, material properties and triggering storm rainfall." Diss., Connect to online resource, 2005. http://wwwlib.umi.com/cr/colorado/fullcit?p1430198.

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Stein, Luiza Paschoal. "Morfodinâmica e eventos de sobrelavagem: praias da baía de Santos, SP." Universidade de São Paulo, 2018. http://www.teses.usp.br/teses/disponiveis/21/21136/tde-15012019-145511/.

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As praias urbanizadas são ambientes complexos devido à interação da ocupação antropogênica e dos processos costeiros. A ocupação costeira vem se caracterizando por alteração e deterioração da paisagem, processo mais intenso em grandes cidades litorâneas, onde casas e edifícios são construídos nas proximidades imediatas da orla. O presente trabalho analisa a morfodinâmica e processo de sobrelavagem das praias de Santos e Itararé, duas praias urbanizadas com a presença de obras na orla. Foram realizados levantamentos topográficos nas praias e modelagem de ondas (Delft 3D - Wave) para toda a baía
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Brodie, Katherine L. "Observations of storm morphodynamics using Coastal Lidar and Radar Imaging System (CLARIS): Importance of wave refraction and dissipation over complex surf-zone morphology at a shoreline erosional hotspot." W&M ScholarWorks, 2010. https://scholarworks.wm.edu/etd/1539616582.

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Elevated water levels and large waves during storms cause beach erosion, overwash, and coastal flooding, particularly along barrier island coastlines. While predictions of storm tracks have greatly improved over the last decade, predictions of maximum water levels and variations in the extent of damage along a coastline need improvement. In particular, physics based models still cannot explain why some regions along a relatively straight coastline may experience significant erosion and overwash during a storm, while nearby locations remain seemingly unchanged. Correct predictions of both the t
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Earlie, Claire Siobhan. "Field observations of wave induced coastal cliff erosion, Cornwall, UK." Thesis, University of Plymouth, 2015. http://hdl.handle.net/10026.1/3526.

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Coastal cliff erosion is a widespread problem that threatens property and infrastructure along many of the world’s coastlines. The management of this risk calls for robust quantification of cliff erosion rates, which are often difficult to obtain along rocky coasts. Quantification of sea-cliff rates of retreat on annual to decadal time scales has typically been limited to rapidly eroding soft rock coastlines. Rates of erosion used for shoreline management in the UK are generally based on analysis of historic maps and aerial photographs which, in rocky coast environments, does not wholly captur
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Hammond, Sean Paul. "Children's story authoring with Propp's morphology." Thesis, University of Edinburgh, 2011. http://hdl.handle.net/1842/5294.

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This thesis applies concepts from Vladimir Propp’s model of the narrative structure of fairy tales (Propp’s morphology) to a story authoring tool for children. A computer story authoring application based on Propp’s morphology is developed and evaluated through empirical studies with children. Propp’s morphology is a promising model of narrative for a children’s story authoring tool, with the potential to give children a powerful mental model with which to construct stories. Recent research has argued for the use of computer-based interactive narrative authoring tools (which enable the constru
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Šáchová, Irena. "Bionika v architektuře (strom jako inspirační zdroj)." Doctoral thesis, Vysoké učení technické v Brně. Fakulta architektury, 2012. http://www.nusl.cz/ntk/nusl-233238.

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The work deals with nature prefigurations, which can be used in architecture. The first part is concerned with the bionics in architecture in general. There are introduced all available pieces of knowledge falling within this branch. The second part is focused on the nature prefiguration – tree. The tree was analyzed from different points of view. Suitable principles, which were found, were transformed to the field of architecture. On the basis of children's drawings the changing approach to “tree as a home” during adolescence was charted. The work can serve as a comprehensive supporting docum
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Conn, Jeffrey C. "Portland Dialect Study: The Story of /æ/ in Portland." PDXScholar, 2000. https://pdxscholar.library.pdx.edu/open_access_etds/4518.

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This study reports on the hypothesized raising of the low, front vowel /æ/, which is characteristic of a regional dialect vowel shift found in cities of the Midwest and Eastern North of the United States. The raising of this vowel is the primary change in a series of vowel shifts that have traditionally been attributed to this region of the U.S. The purpose of this study is to document the production of this vowel by residents of Portland, Oregon, in order to see what light it can shed on dialect research of the Pacific Northwest, especially across age groups to see if it can be implicated in
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Nano, Del Castillo Ariadna. "Impacto entre el visual merchandising y la experiencia que vive el cliente femenino de 18 a 30 años, del sector A/B en las concept store de Morphology en el distrito de Miraflores en el presente año." Universidad Peruana de Ciencias Aplicadas (UPC), 2019. http://hdl.handle.net/10757/626189.

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El e-tailing es una nueva manera de compra que cada vez tiene mayor acogida en el cliente, se estima que en el 2021 las compras online representarán el 15.5% de las ventas de retail, debido a ello la mejor manera de contrarrestar la nueva modalidad de compra es a través del concept store debido a la atmósfera agradable que puede brindar el visual merchandising creando en el cliente una experiencia que no podrá vivirla a través de sus compras por internet. La investigación fue realizada a través del método mixto, llevándose a cabo la recolección y el análisis de datos cuantitativos y cualitat
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Books on the topic "Storm morphology"

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Grim, William Edward. Form, process and morphology in the "Sturm und drang" symphonies of Franz Joseph Haydn. UMI, 1985.

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W, Diggs L., Sturm Dorothy, Bell Ann MS, Sallah Sabah, and Diggs L. W, eds. Diggs, Sturm, Bell the morphology of human blood cells. 7th ed. Abbott Laboratories, 2005.

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Mitchell, Graham. How Giraffes Work. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780197571194.001.0001.

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There are few creatures more beautiful, more aloof, and more fascinating than giraffes. Once they were plentiful and filled African landscapes, but in 2016 they were re-classified from “least concern” to “vulnerable” by the International Union for Conservation of Nature. Their survival in the wild is not assured. Much has been written about their private lives, about their behavior, social biology, and ecology, and their history in art and diplomacy. But so far no book has been written about their private lives, their physiology, and their anatomy and biochemistry—in short, the normal function
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Sweedman, Luke, and David Merritt. Australian Seeds. CSIRO Publishing, 2006. http://dx.doi.org/10.1071/9780643094079.

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This is the first complete guide to the collection, processing and storage of wild collected seed. While the main focus is on Australian seeds, the procedures and protocols described within the book are of international standard and apply to users throughout the world.
 The book provides a basic understanding to seed biology, evolution and morphology, and includes chapters on all aspects of harvesting, processing and storage of seeds. This will enable users to collect, process and store seed more efficiently, thus reducing loss of seed viability during the storage process with potentially
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Book chapters on the topic "Storm morphology"

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Cander, Ljiljana R. "Ionospheric Storm Morphology." In Ionospheric Space Weather. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-99331-7_5.

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Murray, Ian S., Martin Beech, Michael J. Taylor, Peter Jenniskens, and Robert L. Hawkes. "Comparison of 1998 and 1999 Leonid Light Curve Morphology and Meteoroid Structure." In Leonid Storm Research. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-2071-7_26.

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Frahm, R. A., P. H. Reiff, J. D. Winningham, and J. L. Burch. "Banded Ion Morphology: Main and Recovery Storm Phases." In Geophysical Monograph Series. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm038p0098.

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Wang, Ping, and Jun Cheng. "Storm Impacts on the Morphology and Sedimentology of Open-coast Tidal Flats." In Coastal Storms. John Wiley & Sons, Ltd, 2017. http://dx.doi.org/10.1002/9781118937099.ch5.

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Keen, T. R., R. L. Slingerland, S. J. Bentley, Y. Furukawa, W. J. Teague, and J. D. Dykes. "Sediment Transport on Continental Shelves: Storm Bed Formation and Preservation in Heterogeneous Sediments." In Sediments, Morphology and Sedimentary Processes on Continental Shelves. John Wiley & Sons, Ltd, 2013. http://dx.doi.org/10.1002/9781118311172.ch14.

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Li, Michael Z., Edward L. King, and Robert H. Prescott. "Seabed Disturbance and Bedform Distribution and Mobility on the Storm-Dominated Sable Island Bank, Scotian Shelf." In Sediments, Morphology and Sedimentary Processes on Continental Shelves. John Wiley & Sons, Ltd, 2013. http://dx.doi.org/10.1002/9781118311172.ch10.

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Pettersson, Thomas, and D. Lavieille. "Evolution on pollutant removal efficiency in storm water ponds due to changes in pond morphology." In Alliance For Global Sustainability Bookseries. Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-6010-6_37.

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Ruggiero, Peter, Sally Hacker, Eric Seabloom, and Phoebe Zarnetske. "The Role of Vegetation in Determining Dune Morphology, Exposure to Sea-Level Rise, and Storm-Induced Coastal Hazards: A U.S. Pacific Northwest Perspective." In Barrier Dynamics and Response to Changing Climate. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-68086-6_11.

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Wang, Ping, and Tiffany M. Roberts Briggs. "Storm-Induced Morphology Changes along Barrier Islands and Poststorm Recovery." In Coastal and Marine Hazards, Risks, and Disasters. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-396483-0.00010-8.

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Hayden, Bruce P., and Nils R. Hayden. "Decadal and Century-Long Changes in Storminess at Long-Term Ecological Research Sites." In Climate Variability and Ecosystem Response in Long-Term Ecological Research Sites. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195150599.003.0026.

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Ecological disturbances at Long-Term Ecological Research (LTER) sites are often the result of extreme meteorological events. Among the events of significance are tropical storms, including hurricanes, and extratropical cyclones. Extratropical storms are low-pressure systems of the middle and high latitudes with their attendant cold and warm fronts. These fronts are associated with strong, horizontal thermal gradients in surface temperatures, strong winds, and a vigorous jet stream aloft. These storms and their attendant fronts generate most of the annual precipitation in the continental United States and provide the lifting mechanisms for thunderstorms that, on occasion, spawn tornadoes. Off the United States West and East Coasts, extratropical storms generate winds, wind waves, wind tides, and long-shore currents that rework coastal sediments, alter landscape morphology, and change the regional patterns of coastal erosion and accretion (Dolan et al. 1988). Although extratropical storms do not match hurricanes in either precipitation intensity or in the strength of the winds generated, they are much larger in size and have a more extensive geographic impact. On occasion, extratropical storms will intensify at an extraordinary rate of 1 millibar (mb) per hour for 24 hours or more. Such storms are classed as “bomb” and are comparable to hurricanes. Extratropical storms occur in all months of the year but are most frequent and more intense in winter when the north-south temperature contrast is large and dynamic support for storm intensification from the stronger jet stream aloft is great. In this chapter, we will explore the history of storminess for those LTER sites in the continental United States at which more than a century of data on storms and their storm tracks are readily available. Specifically, we will look at the record of changes in storminess at both the regional and national scales. During the 1990s, significant storms along the U.S. West Coast and droughts and fires in Florida in an El Niño year led to a hypothesis that El Niño and La Niña conditions were associated with a modulation in the frequency of storms. In addition, it has been suggested that the frequency of El Niño and La Niña events and, by inference, storminess, has increased during the past century.
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Conference papers on the topic "Storm morphology"

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JOHNSON, BRADLEY D., and KATHERINE L. BRODIE. "MODELING STORM WAVES AND DUNE MORPHOLOGY CHANGE." In International Conference on Coastal Sediments 2019. WORLD SCIENTIFIC, 2019. http://dx.doi.org/10.1142/9789811204487_0113.

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Alexander, Jane, and Jennifer Avila Sanchez. "STATEN ISLAND BEACH MORPHOLOGY - IMPLICATIONS FOR SHORELINE RESPONSE TO STORM EVENTS." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328335.

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Eelkema, M., Z. B. Wang, and A. Hibma. "Ebb-tidal delta morphology in response to a storm surge barrier." In NCK-days 2012 : Crossing borders in coastal research. University of Twente, Department of Water Engineering & Management, 2012. http://dx.doi.org/10.3990/2.184.

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Takewaka, Satoshi, and Hitoshi Nishimura. "WAVE AND MORPHOLOGY OBSERVATION DURING A STORM EVENT WITH A NAUTICAL X-BAND RADAR." In Proceedings of the 2nd International Conference. WORLD SCIENTIFIC, 2004. http://dx.doi.org/10.1142/9789812703040_0141.

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Takewaka, Satoshi. "Intertidal Morphology and Wave Run-Up Observations during a Storm Event with X-Band Nautical Radar." In Fifth International Conference on Coastal Dynamics. American Society of Civil Engineers, 2006. http://dx.doi.org/10.1061/40855(214)62.

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CONLIN, MATTHEW P., PETER N. ADAMS, NATHANIEL G. PLANT, JOHN M. JAEGER, and RICHARD MACKENZIE. "DAILY TO DECADAL VARIABILITY OF BEACH MORPHOLOGY AT NASA-KENNEDY SPACE CENTER: STORM INFLUENCES ACROSS TIMESCALES." In International Conference on Coastal Sediments 2019. WORLD SCIENTIFIC, 2019. http://dx.doi.org/10.1142/9789811204487_0194.

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MacIsaac, Isabella Valentina. "STORM-RELATED CHANGES IN BEACH MORPHOLOGY AND ANALYSIS OF SEDIMENT CHARACTERISTICS, TORREY PINES STATE BEACH, SAN DIEGO COUNTY, SOUTHERN CALIFORNIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-278975.

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Belova, Nataliya, Nataliya Belova, Alisa Baranskaya, et al. "MONITORING OF THE THERMOABRASIONAL AND ACCUMULATIVE COASTS NEAR THE UNDERWATER GAS PIPELINE ROUTE ACROSS THE BAYDARATSKAYA BAY, KARA SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315e92b1a.

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The coasts of Baydaratskaya Bay are composed by loose frozen sediments. At Yamal Peninsula accumulative coasts are predominant at the site where pipeline crosses the coast, while thermoabrasional coast are prevail at the Ural coast crossing site. Coastal dynamics monitoring on both sites is conducted using field and remote methods starting from the end of 1980s. As a result of construction in the coastal zone the relief morphology was disturbed, both lithodynamics and thermal regime of the permafrost within the areas of several km around the sites where gas pipeline crosses coastline was chang
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Belova, Nataliya, Nataliya Belova, Alisa Baranskaya, et al. "MONITORING OF THE THERMOABRASIONAL AND ACCUMULATIVE COASTS NEAR THE UNDERWATER GAS PIPELINE ROUTE ACROSS THE BAYDARATSKAYA BAY, KARA SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b94878a9e64.97890040.

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The coasts of Baydaratskaya Bay are composed by loose frozen sediments. At Yamal Peninsula accumulative coasts are predominant at the site where pipeline crosses the coast, while thermoabrasional coast are prevail at the Ural coast crossing site. Coastal dynamics monitoring on both sites is conducted using field and remote methods starting from the end of 1980s. As a result of construction in the coastal zone the relief morphology was disturbed, both lithodynamics and thermal regime of the permafrost within the areas of several km around the sites where gas pipeline crosses coastline was chang
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Liao, Mei, Hui-Zheng Liu, Wei Jiang, Tao Wang, Yong-Qin Xie, and Shi-Hong Zeng. "Fuel Supply Patterns and Suburban Morphology: Jiaxing's Story." In 2015 International Conference on Energy, Environmental & Sustainable Ecosystem Development (EESED 2015). WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814723008_0122.

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Reports on the topic "Storm morphology"

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Melby, Jeffrey, Thomas Massey, Fatima Diop, et al. Coastal Texas Protection and Restoration Feasibility Study : Coastal Texas flood risk assessment : hydrodynamic response and beach morphology. Engineer Research and Development Center (U.S.), 2021. http://dx.doi.org/10.21079/11681/41051.

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The US Army Corps of Engineers, Galveston District, is executing the Coastal Texas Protection and Restoration Feasibility Study coastal storm risk management (CSRM) project for the region. The project is currently in the feasibility phase. The primary goal is to develop CSRM measures that maximize national net economic development benefits. This report documents the coastal storm water level and wave hazard, including sea level rise, for a variety of flood risk management alternatives. Four beach restoration alternatives for Galveston Island and Bolivar peninsula were evaluated. Suites of synt
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Coastal Lidar And Radar Imaging System (CLARIS) mobile terrestrial lidar survey along the Outer Banks, North Carolina in Currituck and Dare counties. Coastal and Hydraulics Laboratory (U.S.), 2020. http://dx.doi.org/10.21079/11681/39419.

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The Coastal Observation and Analysis Branch (COAB) located at the Field Research Facility (FRF) conducts quarterly surveys and post-storm surveys along up to 60 kilometers of coastline within the vicinity of the FRF to assess, evaluate, and provide updated observations of the morphology of the foreshore and dune system. The surveys are conducted using a mobile terrestrial LiDAR scanner coupled with an Inertial Navigation System (INS). Traditionally the surveys coincide with a low tide, exposing the widest swath of visible sediment to the scanner as well as enough wind-sea swell or texture to i
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Coastal Lidar And Radar Imaging System (CLARIS) mobile terrestrial lidar survey along the Outer Banks, North Carolina in Currituck and Dare counties. Coastal and Hydraulics Laboratory (U.S.), 2020. http://dx.doi.org/10.21079/11681/39419.

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Abstract:
The Coastal Observation and Analysis Branch (COAB) located at the Field Research Facility (FRF) conducts quarterly surveys and post-storm surveys along up to 60 kilometers of coastline within the vicinity of the FRF to assess, evaluate, and provide updated observations of the morphology of the foreshore and dune system. The surveys are conducted using a mobile terrestrial LiDAR scanner coupled with an Inertial Navigation System (INS). Traditionally the surveys coincide with a low tide, exposing the widest swath of visible sediment to the scanner as well as enough wind-sea swell or texture to i
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