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Journal articles on the topic 'Storm Frequency'

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1

Grabowska, Katarzyna. "Changes in Storm Frequency in the Mediterranean Sea Region." Miscellanea Geographica 14, no. 1 (2010): 71–78. http://dx.doi.org/10.2478/mgrsd-2010-0007.

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Abstract Storms in the European part of the Mediterranean Sea Basin are characterized in the paper. Data on storm days comes from the years 1986-2008, from fourteen stations located on the coast and on islands of the Mediterranean Sea (Gibraltar, Valencia, Palma de Majorca, Marseille, Ajaccio – Corsica, Cagliari – Sardinia, Palermo – Sicily, Naples, Luqa – Malta, Thessaloniki, Athens, Souda – Crete, Rhodes Airport – Rhodes and Larnaca – Cyprus). The greatest number of storm days was noted in Corsica (870 - on the average 37,8 per year) and the least in Gibraltar (371 – 16,1). In most of the ex
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Luo, Y., Q. Guo, Y. Zheng, K. P. Garmash, L. F. Chernogor, and S. N. Shulga. "Geospace storm effects on August 5-6, 2019." Kosmìčna nauka ì tehnologìâ 27, no. 2 (2021): 45–69. http://dx.doi.org/10.15407/knit2021.02.045.

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Geospace storms are the synergistically interacting magnetic storms, ionospheric storms, atmospheric storms, and the storms in an electric field of magnetospheric, ionospheric, and atmospheric origins. Geospace storms are very diverse, and no two of them behave exactly the same. Therefore, studying the effects of each new storm becomes an urgent task for us. Such research will reveal both the general laws and individual characteristics of storm processes. The purpose of this paper is to present general information about the geospace storm, the results of the analysis of features of magnetic an
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Croley II, Thomas E. "Climate-Biased Storm-Frequency Estimation." Journal of Hydrologic Engineering 6, no. 4 (2001): 275–83. http://dx.doi.org/10.1061/(asce)1084-0699(2001)6:4(275).

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4

Liu, Maofeng, Gabriel A. Vecchi, James A. Smith, and Hiroyuki Murakami. "Projection of Landfalling–Tropical Cyclone Rainfall in the Eastern United States under Anthropogenic Warming." Journal of Climate 31, no. 18 (2018): 7269–86. http://dx.doi.org/10.1175/jcli-d-17-0747.1.

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Abstract Landfalling–tropical cyclone (TC) rainfall is an important element of inland flood hazards in the eastern United States. The projection of landfalling-TC rainfall under anthropogenic warming provides insight into future flood risks. This study examines the frequency of landfalling TCs and associated rainfall using the GFDL Forecast-Oriented Low Ocean Resolution (FLOR) climate model through comparisons with observed TC track and rainfall over the July–November 1979–2005 seasons. The projection of landfalling-TC frequency and rainfall under the representative concentration pathway (RCP)
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5

Blagoveshchensky, D. V., A. S. Kalishin, and M. A. Sergeyeva. "Space weather effects on radio propagation: study of the CEDAR, GEM and ISTP storm events." Annales Geophysicae 26, no. 6 (2008): 1479–90. http://dx.doi.org/10.5194/angeo-26-1479-2008.

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Abstract. The impact of 14 geomagnetic storms from a list of CEDAR, GEM and ISTP storms, that occurred during 1997–1999, on radio propagation conditions has been investigated. The propagation conditions were estimated through variations of the MOF and LOF (the maximum and lowest operation frequencies) on three high-latitude HF radio paths in north-west Russia. Geophysical data of Dst, Bz, AE as well as some riometer data from Sodankyla observatory, Finland, were used for the analysis. It was shown that the storm impact on the ionosphere and radio propagation for each storm has an individual ch
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Бадин, Владимир, and Vladimir Badin. "Resonant ULF absorption in storm time conditions." Solar-Terrestrial Physics 3, no. 1 (2017): 103–13. http://dx.doi.org/10.12737/article_58f97156b06fa5.51468016.

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The work deals with ULF radar observations of the high-latitude ionosphere. Doppler data from the Norwegian STARE instrument are analyzed for the moderate magnetic storm observed on December 31, 1999–January 01, 2000. Upon averaging the Doppler signals along radar beams, the spectral power of signals is determined for each beam as a function of frequency ranging from 1 to 10 mHz. Sharp drops (about 10 dB) of spectral powers with frequency are found for all radar beams. A variational analysis of spectral powers is carried out by least squares, with power drops being modeled by stepwise profiles
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7

Villarini, Gabriele, Gabriel A. Vecchi, Thomas R. Knutson, Ming Zhao, and James A. Smith. "North Atlantic Tropical Storm Frequency Response to Anthropogenic Forcing: Projections and Sources of Uncertainty." Journal of Climate 24, no. 13 (2011): 3224–38. http://dx.doi.org/10.1175/2011jcli3853.1.

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Abstract The impact of future anthropogenic forcing on the frequency of tropical storms in the North Atlantic basin has been the subject of intensive investigation. However, whether the number of North Atlantic tropical storms will increase or decrease in a warmer climate is still heavily debated and a consensus has yet to be reached. To shed light on this issue, the authors use a recently developed statistical model, in which the frequency of North Atlantic tropical storms is modeled by a conditional Poisson distribution with rate of occurrence parameter that is a function of tropical Atlanti
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8

Wehner, Michael F., G. Bala, Phillip Duffy, Arthur A. Mirin, and Raquel Romano. "Towards Direct Simulation of Future Tropical Cyclone Statistics in a High-Resolution Global Atmospheric Model." Advances in Meteorology 2010 (2010): 1–13. http://dx.doi.org/10.1155/2010/915303.

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We present a set of high-resolution global atmospheric general circulation model (AGCM) simulations focusing on the model's ability to represent tropical storms and their statistics. We find that the model produces storms of hurricane strength with realistic dynamical features. We also find that tropical storm statistics are reasonable, both globally and in the north Atlantic, when compared to recent observations. The sensitivity of simulated tropical storm statistics to increases in sea surface temperature (SST) is also investigated, revealing that a credible late 21st century SST increase pr
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9

Shamsan, Z. A., M. Alammar, A. Alharthy, A. Aldahmash, K. A. Al-Snaie, and A. M. Al-Hetar. "Micrometer and Millimeter Wave P-to-P Links Under Dust Storm Effects in Arid Climates." Engineering, Technology & Applied Science Research 9, no. 4 (2019): 4520–24. http://dx.doi.org/10.48084/etasr.2972.

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A dust storm is the main attenuation factor that can disturb receiving radio signals in arid climate condition as in Saudi Arabia. This paper presents a study on the effect of dust storms on the received radio frequency power in a homogenous environment in the city of Riyadh. A number of micrometer and millimeter wave links have been considered along with several measured dust storm data to investigate the dust storm effects. The results showed that dust storm can critically influence the communication link and this effect grows up as the physical distance between the transmitter and the recei
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10

Yahya, Bashar Muneer, and Dursun Zafer Seker. "The Impact of Dust and Sandstorms in Increasing Drought Areas in Nineveh Province, North-western Iraq." Journal of Asian and African Studies 54, no. 3 (2018): 346–59. http://dx.doi.org/10.1177/0021909618812913.

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According to many local and international reports, the risk of dust and sandstorms has increased significantly in Iraq, creating serious environmental and social problems. In this study Nineveh province was selected as the study area to investigate the relationship between the increase in such storms and drought expansion. In the study, storm-feeding regions and a probable storm path were detected using remote sensing and Geographic Information System (GIS). Standardized Precipitation Index (SPI) and runoff values were estimated and gathered as supplementary data with rainfall, temperature and
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11

Luo, Yiyang, Leonid Chernogor, Kostiantyn Garmash, Qiang Guo, Victor Rozumenko, and Yu Zheng. "Dynamic processes in the magnetic field and in the ionosphere during the 30 August–2 September 2019 geospace storm: influence on high frequency radio wave characteristics." Annales Geophysicae 39, no. 4 (2021): 657–85. http://dx.doi.org/10.5194/angeo-39-657-2021.

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Abstract. The concept that geospace storms are comprised of synergistically coupled magnetic storms, ionospheric storms, atmospheric storms, and storms in the electric field originating in the magnetosphere, the ionosphere, and the atmosphere (i.e., electrical storms) was validated a few decades ago. Geospace storm studies require the employment of multiple-method approaches to the Sun–interplanetary medium–magnetosphere–ionosphere–atmosphere–Earth system. This study provides general analysis of the 30 August–2 September 2019 geospace storm, the analysis of disturbances in the geomagnetic fiel
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12

Jun, Changhyun, Xiaosheng Qin, Yeou-Koung Tung, and Carlo De Michele. "Storm event-based frequency analysis method." Hydrology Research 49, no. 3 (2017): 700–710. http://dx.doi.org/10.2166/nh.2017.175.

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Abstract In this study, a storm event-based frequency analysis method was proposed to mitigate the limitations of conventional rainfall depth–duration–frequency (DDF) analysis. The proposed method takes the number, rainfall depth, and duration of rainstorm events into consideration and is advantageous in estimation of more realistic rainfall quantiles for a given return period. For the purpose of hydraulics design, the rainfall depth thresholds are incorporated to retrieve the rainstorm events for estimating design rainfalls. The proposed method was tested against the observed rainfall data fr
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13

Золотухина, Нина, Nina Zolotukhina, Владимир Куркин, Vladimir Kurkin, Неля Полех, and Nelya Polekh. "Ionospheric disturbances over East Asia during intense December magnetic storms of 2006 and 2015: similarities and differences." Solar-Terrestrial Physics 4, no. 3 (2018): 28–42. http://dx.doi.org/10.12737/stp-43201805.

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Using data from ionosondes, located in East Asia, and total electron content maps, we have made a comparative analysis of ionospheric disturbances associated with the intense geomagnetic storms of December 14–16, 2006 and December 19–22, 2015. These storms had almost equal peak intensities (Dstmin=–162 and –155 nT), but different durations of the main phases (2.5 and 19 hr). At the beginning of both the storms, the region under study was located in the vicinity of the midnight meridian. Ionospheric responses to magnetic storms differed in: i) an increase in the F2-layer critical frequency at s
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14

Yang, Ji, Kun Zhao, Xingchao Chen, Anning Huang, Yuanyuan Zheng, and Kangyuan Sun. "Subseasonal and Diurnal Variability in Lightning and Storm Activity over the Yangtze River Delta, China, during Mei-yu Season." Journal of Climate 33, no. 12 (2020): 5013–33. http://dx.doi.org/10.1175/jcli-d-19-0453.1.

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AbstractUsing 5 years of operational Doppler radar, cloud-to-ground (CG) lightning observations, and National Centers for Environmental Prediction reanalysis data, this study examined the spatial and temporal characteristics of and correlations between summer storm and lightning activity over the Yangtze River Delta (YRD), with a focus on subseasonal variability and diurnal cycles. The spatiotemporal features of storm top, duration, maximum reflectivity, size, and cell-based vertical integrated liquid water were investigated using the Storm Cell Identification and Tracking algorithm. Our resul
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15

Babcock, Jeffrey M., Barry A. Kirkendall, and John A. Orcutt. "Relationships between ocean bottom noise and the environment." Bulletin of the Seismological Society of America 84, no. 6 (1994): 1991–2007. http://dx.doi.org/10.1785/bssa0840061991.

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Abstract Observations of ocean bottom low-frequency noise and surface environmental data over a period of 27 days in the northern Atlantic during the SAMSON and SWADE experiments reveal how closely related the noise is to meteorological conditions. Double-frequency microseisms produced by nonlinear interactions of storm-induced surface gravity waves are especially evident in the frequency band 0.16 to 0.3 Hz and show a high variability in both amplitude and peak frequencies. Bifurcated at times, the peak that characterizes the microseism band contains local and distant or “teleseismic” compone
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16

Watt, W. E., K. C. A. Chow, W. D. Hogg, and K. W. Lathem. "A 1-h urban design storm for Canada." Canadian Journal of Civil Engineering 13, no. 3 (1986): 293–300. http://dx.doi.org/10.1139/l86-041.

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The advent of stormwater modelling techniques has resulted in the need for a Canadian urban design storm. As a first stage in meeting this need, a 1-h urban design storm has been developed. This design storm, which is fully described by two parameters and the rainfall depth as given by Atmospheric Environment Service (AES) intensity–duration–frequency data, is specified for a wide range of return periods for all regions of Canada. Extensive comparisons with observed 1-h storms, both in the temporal domain and the frequency domain, indicate that the two-parameter mathematical model is capable o
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17

Weiss, Jérôme, Pietro Bernardara, and Michel Benoit. "ASSESSMENT OF THE REGIONAL FREQUENCY ANALYSIS TO THE ESTIMATION OF EXTREME STORM SURGES." Coastal Engineering Proceedings 1, no. 33 (2012): 27. http://dx.doi.org/10.9753/icce.v33.management.27.

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Regional frequency analysis (RFA) is performed to estimate extreme storm surges along the French coasts of the Atlantic Ocean, the English Channel and the Southern part of the North Sea. An insight on the formation of physically homogeneous regions from a criterion of propagation of storms is provided. The treatment of the pairwise dependence structure within a given region through a spatial extreme value copula is also considered, leading to a model coupling physically-based RFA and spatial dependence to describe the probabilistic behavior of extreme storm surges.
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18

Weisse, Ralf, Hans von Storch, and Frauke Feser. "Northeast Atlantic and North Sea Storminess as Simulated by a Regional Climate Model during 1958–2001 and Comparison with Observations." Journal of Climate 18, no. 3 (2005): 465–79. http://dx.doi.org/10.1175/jcli-3281.1.

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Abstract An analysis of the storm climate of the northeast Atlantic and the North Sea as simulated by a regional climate model for the past 44 yr is presented. The model simulates the period 1958–2001 driven by the National Centers for Environmental Prediction–National Center for Atmospheric Research (NCEP–NCAR) reanalysis. Comparison with observations shows that the model is capable of reproducing impact-related storm indices such as the number of severe and moderate storms per year or the total number of storms and upper intra-annual percentiles of near-surface wind speed. The indices descri
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19

Tang, Xu, Jia, Luo, and Shao. "Estimating Errors in Sizing LID Device and Overflow Prediction Using the Intensity-Duration-Frequency Method." Water 11, no. 9 (2019): 1853. http://dx.doi.org/10.3390/w11091853.

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Low impact development (LID) devices or green infrastructures have been advocated for urban stormwater management worldwide. Currently, the design and evaluation of LID devices adopt the Intensity-Duration-Frequency (IDF) method, which employs the average rainfall intensity. However, due to variations of rainfall intensity during a storm event, using average rainfall intensity may generate certain errors when designing a LID device. This paper presents an analytical study to calculate the magnitude of such errors with respect to LID device design and associated device performance evaluation. T
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20

Middleton, Nick. "Variability and Trends in Dust Storm Frequency on Decadal Timescales: Climatic Drivers and Human Impacts." Geosciences 9, no. 6 (2019): 261. http://dx.doi.org/10.3390/geosciences9060261.

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Dust storms present numerous hazards to human society and are particularly significant to people living in the Dust Belt which stretches from the Sahara across the Middle East to northeast Asia. This paper presents a review of dust storm variability and trends in frequency on decadal timescales from three Dust Belt settlements with long-term (>50 years) meteorological records: Nouakchott, Mauritania; Zabol, Iran, and Minqin, China. The inhabitants of each of these settlements have experienced a decline in dust storms in recent decades, since the late 1980s at Nouakchott, since 2004 at Zabol
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Thompson, Philip R., Gary T. Mitchum, Cedric Vonesch, and Jianke Li. "Variability of Winter Storminess in the Eastern United States during the Twentieth Century from Tide Gauges." Journal of Climate 26, no. 23 (2013): 9713–26. http://dx.doi.org/10.1175/jcli-d-12-00561.1.

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Interannual to multidecadal variability of winter storminess in the eastern United States was studied using water level measurements from coastal tide gauges. The proximity to the coast of the primary winter storm track in the region allows the use of tide gauges to study temporal modulations in the frequency of these storms. Storms were identified in high-passed, detided sea level anomalies in 20 gauges from all coasts of North America to assess variability in winter storminess along particular storm tracks. The primary result is a significant multidecadal increase in the number of storms aff
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Albugami, Sarah, Steven Palmer, Jonathan Cinnamon, and Jeroen Meersmans. "Spatial and Temporal Variations in the Incidence of Dust Storms in Saudi Arabia Revealed from In Situ Observations." Geosciences 9, no. 4 (2019): 162. http://dx.doi.org/10.3390/geosciences9040162.

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Monthly meteorological data from 27 observation stations provided by the Presidency of Meteorology and Environment (PME) of Saudi Arabia were used to analyze the spatial and temporal distribution of atmospheric dust in Saudi Arabia between 2000 and 2016. These data were used to analyze the effects of environmental forcing on the occurrence of dust storms across Saudi Arabia by considering the relationships between dust storm frequency and temperature, precipitation, and wind variables. We reveal a clear seasonality in the reported incidence of dust storms, with the highest frequency of events
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Rangari, Vinay Ashok, and Sriramoju Sai Prashanth. "Simulation of Urban Drainage System Using a Storm Water Management Model (SWMM)." Asian Journal of Engineering and Applied Technology 7, no. 1 (2018): 7–10. http://dx.doi.org/10.51983/ajeat-2018.7.1.872.

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Urban floods are caused due to increase in population density, development of urban infrastructure without paying due consideration to drainage aspects and increase in paved surfaces. Storm water modelling plays an important role in checking issues such as flash floods and urban water-quality problems. The SWMM (Storm Water Management Model) has been an effective tool for simulating floods in urban areas. In this study a SWMM model is developed to analyze drainage network for the campus of National Institute of Technology, Warangal in the city of Warangal, Telangana, India. The model is simula
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Rudlosky, Scott D., and Henry E. Fuelberg. "Documenting Storm Severity in the Mid-Atlantic Region Using Lightning and Radar Information." Monthly Weather Review 141, no. 9 (2013): 3186–202. http://dx.doi.org/10.1175/mwr-d-12-00287.1.

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Abstract Storm severity in the mid-Atlantic region of the United States is examined using lightning, radar, and model-derived information. Automated Warning Decision Support System (WDSS) procedures are developed to create grids of lightning and radar parameters, cluster individual storm features, and data mine the lightning and radar attributes of 1252 severe and nonsevere storms. The study first examines the influence of serial correlation and uses autocorrelation functions to document the persistence of lightning and radar parameters. Decorrelation times are found to vary by parameter, stor
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Золотухина, Нина, Nina Zolotukhina, Владимир Куркин, Vladimir Kurkin, Неля Полех, and Nelya Polekh. "Ionospheric disturbances over East Asia during intense December magnetic storms of 2006 and 2015: similarities and differences." Solnechno-Zemnaya Fizika 4, no. 3 (2018): 39–56. http://dx.doi.org/10.12737/szf-43201805.

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Using data from ionosondes, located in East Asia, and total electron content maps, we have made a comparative analysis of ionospheric disturbances as-sociated with the intense geomagnetic storms of De-cember 14–16, 2006 and December 19–22, 2015. These storms had almost equal peak intensities (Dstmin=–162 and –155 nT), but different durations of the main phases (2.5 and 19 hr). At the beginning of both the storms, the region under study was located in the vicinity of the midnight meridian. Ionospheric re-sponses to magnetic storms differed in: i) an increase in the F2-layer critical frequency a
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26

Hu, S., A. Bhattacharjee, J. Hou, et al. "Ionospheric storm forecast for high-frequency communications." Radio Science 33, no. 5 (1998): 1413–28. http://dx.doi.org/10.1029/98rs02219.

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27

GORNISH, ELISE S., and THOMAS E. MILLER. "Effects of storm frequency on dune vegetation." Global Change Biology 16, no. 10 (2010): 2668–75. http://dx.doi.org/10.1111/j.1365-2486.2009.02144.x.

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28

Osman Akan, A. "Derived Frequency Distribution for Storm Runoff Pollution." Journal of Environmental Engineering 114, no. 6 (1988): 1344–51. http://dx.doi.org/10.1061/(asce)0733-9372(1988)114:6(1344).

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Zhao, Ming, and Isaac M. Held. "TC-Permitting GCM Simulations of Hurricane Frequency Response to Sea Surface Temperature Anomalies Projected for the Late-Twenty-First Century." Journal of Climate 25, no. 8 (2012): 2995–3009. http://dx.doi.org/10.1175/jcli-d-11-00313.1.

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Abstract A tropical cyclone–permitting global atmospheric model is used to explore the hurricane frequency response to sea surface temperature (SST) anomalies generated by coupled models for the late-twenty-first century. Results are presented for SST anomalies averaged over 18 models as well as from 8 individual models. For each basin, there exists large intermodel spread in the magnitude and even the sign of the frequency response among the different SST projections. These sizable variations in response are explored to understand features of SST distributions that are important for the basin
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Corte, Guilherme N., Thomas A. Schlacher, Helio H. Checon, et al. "Storm effects on intertidal invertebrates: increased beta diversity of few individuals and species." PeerJ 5 (May 23, 2017): e3360. http://dx.doi.org/10.7717/peerj.3360.

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Climate change is predicted to lead to more extreme weather events, including changes to storm frequency, intensity and location. Yet the ecological responses to storms are incompletely understood for sandy shorelines, the globe’s longest land-ocean interface. Here we document how storms of different magnitude impacted the invertebrate assemblages on a tidal flat in Brazil. We specifically tested the relationships between wave energy and spatial heterogeneity, both for habitat properties (habitat heterogeneity) and fauna (β-diversity), predicting that larger storms redistribute sediments and h
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Jimme, M. A., A. L. Disa, and M. B. Ngamdu. "Human Perception on the Effects of Dust Storm on the Health of Residents’ of Damaturu Metropolis, Yobe State." Nigerian Journal of Environmental Sciences and Technology 4, no. 2 (2020): 421–31. http://dx.doi.org/10.36263/nijest.2020.02.0129.

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Dust storms are among nature’s most violent and unpredictable phenomena. High winds lift dirt or sand particles into the air, unleashing a turbulent, suffocating cloud that reduces visibility to almost nothing in a matter of seconds and cause property damage, injuries, and deaths. Damaturu Metropolis has been experiencing dust storm most frequently more especially during the onset of the rainy season. The study examined the human perception on the effects of dust storm on the health of residents’ of Damaturu metropolis with the aim of identifying and examining the causes, frequency, effects of
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32

Scharffenberg, Kevin C., Dustin Whalen, Shannon A. MacPhee, et al. "Oceanographic, ecological, and socio-economic impacts of an unusual summer storm in the Mackenzie Estuary." Arctic Science 6, no. 2 (2020): 62–76. http://dx.doi.org/10.1139/as-2018-0029.

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With increased warming and open water due to climate change, the frequency and intensity of storm surges is expected to increase. Although studies have shown that strong storms can negatively impact Arctic ecosystems, the impact of storms on Arctic marine mammals is relatively unknown. In July 2016, an unusually large storm occurred in the Mackenzie Delta while instrumented seabed moorings equipped with hydrophones and oceanographic sensors were in place to study environmental drivers of beluga habitat use during their summer aggregation. The storm lasted up to 88 h, with maximum wind speeds r
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Butler, H. Lee, and Mark D. Prater. "INNOVATIVE DETERMINATION OF NEARSHORE FLOOD FREQUENCY." Coastal Engineering Proceedings 1, no. 20 (1986): 181. http://dx.doi.org/10.9753/icce.v20.181.

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Reliable estimates of coastal flooding from tides and storm surges are required for making sound engineering decisions regarding the design, operation and maintenance of many coastal projects. A recent investigation of flood frequency along the coast and within the bays of southern Long Island, New York, produced new and optimal approaches to obtain meaningful statistical estimates of flood levels. This paper summarizes various elements of the study and concentrates on the problem of stage-frequency computations in the inland bay areas. Methods for optimizing the number of necessary storm/tide
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Wilson, Larry L., and Efi Foufoula‐Georgiou. "Regional Rainfall Frequency Analysis via Stochastic Storm Transposition." Journal of Hydraulic Engineering 116, no. 7 (1990): 859–80. http://dx.doi.org/10.1061/(asce)0733-9429(1990)116:7(859).

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35

Scheffner, Norman W., Leon E. Borgman, and David J. Mark. "Empirical Simulation Technique Based Storm Surge Frequency Analyses." Journal of Waterway, Port, Coastal, and Ocean Engineering 122, no. 2 (1996): 93–101. http://dx.doi.org/10.1061/(asce)0733-950x(1996)122:2(93).

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Fraedrich, Klaus, Edilbert Kirk, Ute Luksch, and Frank Lunkeit. "The portable university model of the atmosphere (PUMA): Storm track dynamics and low-frequency variability." Meteorologische Zeitschrift 14, no. 6 (2005): 735–45. http://dx.doi.org/10.1127/0941-2948/2005/0074.

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Medina-Elizalde, Martín, Josué Moises Polanco-Martínez, Fernanda Lases-Hernández, Raymond Bradley, and Stephen Burns. "Testing the “tropical storm” hypothesis of Yucatan Peninsula climate variability during the Maya Terminal Classic Period." Quaternary Research 86, no. 2 (2016): 111–19. http://dx.doi.org/10.1016/j.yqres.2016.05.006.

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AbstractWe examine the “tropical storm” hypothesis that precipitation variability in the Yucatan Peninsula (YP) was linked to the frequency of tropical cyclones during the demise of the Classic Maya civilization, in the Terminal Classic Period (TCP, AD 750—950). Evidence that supports the hypothesis includes: (1) a positive relationship between tropical storm frequency and precipitation amount over the YP today (proof of feasibility), (2) a statistically significant correlation between a stalagmite (Chaac) quantitative precipitation record from the YP and the number of named tropical cyclones
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38

Lombardo, Kelly. "Squall Line Response to Coastal Mid-Atlantic Thermodynamic Heterogeneities." Journal of the Atmospheric Sciences 77, no. 12 (2020): 4143–70. http://dx.doi.org/10.1175/jas-d-20-0044.1.

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AbstractIdealized 3D numerical simulations are used to quantify the impact of moving marine atmospheric boundary layers (MABLs) on squall lines in an environment representative of the U.S. mid-Atlantic coastal plain. Characteristics of the MABL, including depth and potential temperature, are varied. Squall lines are most intense while moving over the deepest MABLs, while the storm encountering no MABL is the weakest. Storm intensity is only sensitive to MABL temperature when the MABL is sufficiently deep. Collisions between the storm cold pools and MABLs transition storm lift from surface-base
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Ivanova, A. R., E. N. Skriptunova, N. I. Komasko, and A. A. Zavialova. "Impact of dust and sand storms on the aviation operation and assessment of conditions for their occurrence at aerodromes in European Russia." Hydrometeorological research and forecasting 4 (December 2020): 78–95. http://dx.doi.org/10.37162/2618-9631-2020-4-78-95.

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A review of literature on the impact of dust and sand storms on the air transport operation is presented. Observational data on dust storms at the aerodromes of European Russia for the period of 2001-2019 are analyzed. The seasonal variations in dust transport episodes at aerodromes and its relationship with visibility changes are discussed. The characteristics of dusty air masses and advection are given. It is concluded that the frequency of dust transfer episodes for the aerodromes under study has decreased over the past five years, except for Gumrak aerodrome (Volgograd). Keywords: dust sto
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Tahvildari, Navid, Akash Sahu, Yawen Shen, Mohamed Morsy, and Jonathan Goodall. "COMBINED EFFECT OF STORM SURGE AND OVERLAND FLOW ON FLOODING IN A COASTAL URBAN AREA." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 52. http://dx.doi.org/10.9753/icce.v36.currents.52.

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The coastal regions in the U.S. East Coast and the Gulf of Mexico are under the risk of storm surge and precipitation-driven flooding. The adverse impacts of climate change including sea level rise (SLR), potential increase in intensity and frequency of extreme storms, and increase in precipitation intensity increases the vulnerability of coastal communities to flooding. The common practice for flood hazard assessment in urban coastal areas can result in some errors as the effect of storm surge and overland flow are not considered simultaneously. In this study, we combine the results of two hy
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Andersen, Mikkel René, Elvira de Eyto, Mary Dillane, Russell Poole, and Eleanor Jennings. "13 Years of Storms: An Analysis of the Effects of Storms on Lake Physics on the Atlantic Fringe of Europe." Water 12, no. 2 (2020): 318. http://dx.doi.org/10.3390/w12020318.

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While winter storms are generally common in western Europe, the rarer summer storms may result in more pronounced impacts on lake physics. Using long-term, high frequency datasets of weather and lake thermal structure from the west of Ireland (2005 to 2017), we quantified the effects of storms on the physical conditions in a monomictic, deep lake close to the Atlantic Ocean. We analysed a total of 227 storms during the stratified (May to September, n = 51) and non-stratified (November to March, n = 176) periods. In winter, as might be expected, changes were distributed over the entire water co
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Gaál, L., P. Molnar, and J. Szolgay. "Selection of intense rainfall events based on intensity thresholds and lightning data in Switzerland." Hydrology and Earth System Sciences 18, no. 5 (2014): 1561–73. http://dx.doi.org/10.5194/hess-18-1561-2014.

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Abstract. This paper presents a method to identify intense warm season storms with convective character based on intensity thresholds and the presence of lightning, and analyzes their statistical properties. Long records of precipitation and lightning data at 4 stations and 10 min resolution in different climatological regions in Switzerland are used. Our premise is that thunderstorms associated with lightning generate bursts of high rainfall intensity. We divided all recorded storms into those accompanied by lightning and those without lightning and found the threshold I* that separates inten
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Gaal, L., P. Molnar, and J. Szolgay. "Selection of intense rainfall events based on intensity thresholds and lightning data in Switzerland." Hydrology and Earth System Sciences Discussions 11, no. 1 (2014): 593–628. http://dx.doi.org/10.5194/hessd-11-593-2014.

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Abstract. This paper presents a method to identify intense warm season storms of convective character based on intensity thresholds and lightning, and analyzes their statistical properties. Long records of precipitation and lightning data at 4 stations and 10 min resolution in different climatological regions in Switzerland are used. Our premise is that thunderstorms associated with lightning generate bursts of high rainfall intensity. We divided all storms into those accompanied by lightning and those without lightning and found the threshold I* that separates intense events based on peak 10
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Eichler, Timothy, and Wayne Higgins. "Climatology and ENSO-Related Variability of North American Extratropical Cyclone Activity." Journal of Climate 19, no. 10 (2006): 2076–93. http://dx.doi.org/10.1175/jcli3725.1.

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Abstract The climatology and interannual variability of North American extratropical cyclones are examined using 6-hourly sea level pressure data from the NCEP–NCAR reanalysis for the period 1950–2002 and ECMWF 40-yr Re-Analysis (ERA-40) data from 1971 to 2000. The climatology includes an evaluation of the seasonal frequency and intensity of storms as well as an analysis of extreme event intensity. ENSO variability is evaluated by ENSO phase with emphasis on boreal winter. Results show an enhanced East Coast storm track during El Niño as well as an equatorward shift in storm tracks in the Nort
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De Michele, C., N. T. Kottegoda, and R. Rosso. "IDAF (intensity-duration-area frequency) curves of extreme storm rainfall: a scaling approach." Water Science and Technology 45, no. 2 (2002): 83–90. http://dx.doi.org/10.2166/wst.2002.0031.

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Intensity-duration-area frequency curves, IDAF, are determined for the evaluation of design storms using a scaling approach. The variability of maximum annual rainfall intensity in area and duration is represented through the scaling properties in time and space. Thus the scaling relationships of mean rainfall intensity with area and duration are derived using the concepts of dynamic scaling and statistical self-affinity. For a lognormal distribution of rainfall intensity a multiscaling lognormal model is obtained. This gives the IDAF curves of extreme storm rainfall. An application is made to
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Ghofrani, Zahra, Victor Sposito, and Robert Faggian. "Designing a Pond and Evaluating its Impact Upon Storm-Water Quality and Flow: A Case Study in Rural Australia." Ecological Chemistry and Engineering S 26, no. 3 (2019): 475–91. http://dx.doi.org/10.1515/eces-2019-0036.

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Abstract Storm-water management is a common concern in rural catchments where development-related growth causes increases of storm-water flows. Greater magnitude and frequency of storm-water create greater challenges for mitigating storm-water damage and improving water quality. The concept of Blue-Green Infrastructure (BGI) as a solution incorporates a wide range of applicable components with the aim of minimizing the effect of catchment development on flow regimes without changing the watershed morphology. BGI components manage storm-water by decreasing impermeable cover and expanding natura
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Li, Harrison, and Brian A. Colle. "Multidecadal Changes in the Frequency and Ambient Conditions of Warm Season Convective Storms over the Northeastern United States." Journal of Climate 27, no. 19 (2014): 7285–300. http://dx.doi.org/10.1175/jcli-d-13-00785.1.

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Abstract Long-term changes in warm season (April–September) convective storm frequency over the northeastern United States (NEUS) and the environmental conditions favoring such storms are explored from 1979 to 2010. Linear discriminant analysis (LDA) was used to create thresholds for predicting annual warm season convective storm frequency over various small regions of the NEUS by relating the convective precipitation fields from the North American Regional Reanalysis (NARR) and the Climate Forecast System Reanalysis (CFSR) along with reflectivity data from the National Operational Weather Rad
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Бадин, Владимир, and Vladimir Badin. "Resonant ULF absorption at storm time conditions." Solnechno-Zemnaya Fizika 3, no. 1 (2017): 79–87. http://dx.doi.org/10.12737/21428.

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The work deals with ULF radar observations of the high-latitude ionosphere. Doppler data from the Norwegian STARE instrument are analyzed for the moderate magnetic storm observed on December 31, 1999–January 01, 2000. Upon averaging the Doppler signals along radar beams, the spectral power of signals is determined for each beam as a function of frequency ranging from 1 to 10 mHz. Sharp drops (about 10 dB) of spectral powers with frequency are found for all radar beams. A variational analysis of spectral powers is carried out by least squares, with power drops being modeled by stepwise profiles
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MUNGOV, G., and P. DANIEL. "Storm surges in the Western Black Sea. Operational forecasting." Mediterranean Marine Science 1, no. 1 (2000): 45. http://dx.doi.org/10.12681/mms.4.

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The frequency of the storm surges in the Black Sea is lower than that in other regions of the World Ocean but they cause significant damages as the magnitude of the sea level set-up is up to 7-8 times greater than that of other sea level variations. New methods and systems for storm surge forecasting and studying their statistical characteristics are absolutely necessary for the purposes of the coastal zone management. The operational forecasting storm surge model of Meteo-France was adopted for the Black Sea in accordance with the bilateral agreement between Meteo-France and NINMH. The model
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He, J., C. Valeo, and F. J. C. Bouchart. "Enhancing urban infrastructure investment planning practices for a changing climate." Water Science and Technology 53, no. 10 (2006): 13–20. http://dx.doi.org/10.2166/wst.2006.292.

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Climate change raises many concerns for urban water management because of the effects on all aspects of the hydrological cycle. Urban water infrastructure has traditionally been designed using historical observations and assuming stationary climatic conditions. The capability of this infrastructure, whether for storm-water drainage, or water supply, may be over- or under-designed for future climatic conditions. In particular, changes in the frequency and intensity of extreme rainfall events will have the most acute effect on storm-water drainage systems. Therefore, it is necessary to take futu
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