scispace - formally typeset
Search or ask a question

How do the typhoon wind speed influence storm surge? 


Best insight from top research papers

Typhoon wind speed significantly influences storm surge. Studies have shown that the maximum wind speed of a typhoon plays a crucial role in determining the intensity of the storm surge. Higher wind speeds lead to increased storm surge heights, with a near-linear relationship observed between maximum wind speed and storm surge magnitude. Additionally, the radius of the maximum wind speed (Rmax) of a typhoon also affects storm surge height, with larger typhoons causing higher peak storm surges. The translation speed of a typhoon is another factor to consider, as rapid translation speeds can induce storm surge resonance phenomena, amplifying the impact on coastal areas. Therefore, understanding and accurately predicting typhoon wind speeds are crucial for forecasting and mitigating the effects of storm surges.

Answers from top 5 papers

More filters
Papers (5)Insight
Typhoon wind speed directly impacts storm surge, with higher wind speeds leading to more severe storm surges, as shown in the study on Typhoon Muifa and Typhoon Lekima.
Typhoon wind speed, including central low pressures and forward speed, significantly impacts storm surge magnitude, as seen in the record-breaking storm surge caused by Typhoon Haiyan in the Philippines.
Typhoon wind speed influences storm surge by affecting the intensity and extent of inundation, with higher wind speeds leading to larger storm surge areas and potentially negative surges in certain sea areas.
Typhoon size, not just wind speed, impacts storm surge. Larger typhoons generate higher storm surges, crucial for accurate forecasting, as shown in Tokyo Bay simulations and historical data.
QuikSCAT wind data assists in determining maximum wind speed radii, improving storm surge simulations by assimilating accurate storm surge forcing fields, resulting in closer approximation to observations.

Related Questions

What are the primary factors that contribute to the formation of storm surges in the South China Sea?4 answersThe formation of storm surges in the South China Sea is primarily influenced by multiple factors. These include the warmer sea surface temperatures and lifted mean sea levels due to global warming, leading to more intense tropical cyclones and subsequently more ferocious storm surges. Additionally, the intensity and size of typhoons play a crucial role in the generation of storm surges, with larger typhoons and higher intensities contributing significantly to increased storm surge levels. Furthermore, the frequency and tracks of tropical cyclones are projected to change, leading to a rise in extreme sea levels and storm surges along the coastlines of southern China and Vietnam. The interaction between the atmosphere and the ocean, facilitated by the sea-air coupling, is also essential in accurately predicting and simulating storm surges induced by typhoons in the region.
How do the northeast monsoon and typhoon wind speed influence each other in terms of storm surge?5 answersThe interaction between the northeast monsoon and typhoon wind speed significantly impacts storm surge. Research shows that non-stationarity exists in both typhoon and monsoon wind speeds, with stronger non-stationarity in typhoon wind speed. Typhoon intensity factors, such as maximum wind speed and translation speed, play a crucial role in storm surge generation, with storm surge showing a positive correlation with the distance of the typhoon's center. Additionally, the size of a typhoon, represented by the radius of the maximum wind, influences peak storm surge height, with larger typhoons leading to higher surge heights, especially in semi-enclosed areas like Tokyo Bay. Understanding these dynamics is essential for accurate storm surge forecasting and disaster mitigation efforts.
How do typhoon parameters affect the behavior of typhoon-induced surge?5 answersTyphoon parameters significantly influence the behavior of typhoon-induced surges. Factors such as maximum wind speed, radius of maximum wind speed, and translation speed play crucial roles. The storm surge's magnitude correlates positively with the distance of the typhoon's center, showing near-linear growth with maximum wind speed but decreasing with the radius of maximum wind growth rate. Additionally, the inundation range expands with increasing typhoon intensity, with more intense typhoons causing larger areas of inundation. Typhoon translation speed can lead to a storm surge resonance phenomenon, affecting surge behavior at specific coastal areas. Understanding these parameters is vital for predicting and assessing the impact of typhoon-induced surges accurately.
How does typhoon impact biodiversity?5 answersTyphoons have a significant impact on biodiversity. They can alter the distribution and diversity of fishery resources, leading to changes in the abundance and catch of fish species. Typhoons also play a role in butterfly diversity and community changes, although land-use change has a greater negative impact on butterfly diversity. In temperate coastal bays, typhoons can trigger changes in the species composition, catch amount, and diversity of fish assemblages. Ecological communities in terrestrial habitats show divergent responses to typhoons, with increased spatial variability of biological sound production and individual species detections. Typhoons can also have a dramatic impact on montane freshwater fish populations, leading to declines in density and biodiversity. Overall, typhoons can disrupt ecosystems and have both positive and negative effects on biodiversity depending on the specific habitat and species involved.
How Typhoon caused rainfall occured?4 answersTyphoons cause rainfall through various mechanisms. One factor is the interaction between the typhoon and the local topography. The mountainous regions can enhance precipitation on the windward side and summits of the mountains through orographic uplift. Another factor is the redevelopment of remnant clouds, which leads to the sudden heavy rainfall. This redevelopment is caused by the rapid growth of micro/mesoscale convective systems (MCSs) due to convective instability and frontogenesis. Additionally, the thermodynamic shear advection parameter, which combines convective vorticity, horizontal divergence, and vertical gradient of generalized potential temperature, can predict and indicate the rainfall area and the initiation and evolution of precipitation systems. The intensity of the typhoon, the presence of cold air, and the humidity field also play a role in influencing the amount and distribution of rainfall.
What is typhoon?3 answersA typhoon is a highly organized storm system that develops from initial cyclone eddies and matures by sucking up large quantities of water vapor from warm tropical oceans. This condensation of water vapor at higher altitudes releases latent heat of condensation, which is the primary source of energy that strengthens the typhoon as it moves across the Pacific Ocean. Typhoons are one of the most serious natural disasters that occur annually on China's southeast coast. They are characterized by extreme wind speeds and pose a significant hazard to the region. In the context of wireless sensor networks, Typhoon is a protocol designed to reliably deliver large objects to all nodes of the network. It utilizes spatially-tuned timers, prompt retransmissions, and frequency diversity to reduce contention and promote efficient dissemination of data. Additionally, there is a design theory for utilizing typhoons as a source of wind power generation. This involves designing wind generating units that can harness the high wind speeds and forces associated with typhoons. Experimental studies have also been conducted to understand the dynamic characteristics of typhoons, including their helical structures and soliton-like behavior.

See what other people are reading

What is the objectives of mini fans?
4 answers
The objectives of mini fans are multifaceted based on the designs and features they offer. Mini fans aim to provide portable cooling solutions while incorporating innovative functionalities. These objectives include energy efficiency and environmental friendliness through features like solar charging panels, air purification capabilities using filter layers like electrostatic cotton and activated carbon, hands-free operation and adjustable wind direction for user convenience, enhanced air power and noise reduction through dual fan blades, and versatile usability with multipurpose supporting bases for various elevation angles and air outlet functions. Overall, mini fans strive to offer compact, efficient, and user-friendly cooling solutions with added features for improved functionality and convenience.
How are (period), (circular frequency, and (linear frequency related to each other?
5 answers
The relationship between period, circular frequency, and linear frequency can be understood through various signal processing and analysis techniques. Circular frequency, as defined in Context_2, is related to the instantaneous frequency of a signal's trajectory on the phase plane. In contrast, linear frequency is a more traditional concept used in signal analysis. The period of a signal, as discussed in Context_5, is crucial for understanding the dynamics of systems subject to external disturbances. While circular frequency and linear frequency are more directly related to the signal's characteristics, the period provides essential information about the time intervals and behavior of the system. Integrating these concepts can enhance the analysis of signals and systems in various engineering applications, as highlighted in the different contexts provided.
Are coastal winds the strongest?
5 answers
Coastal winds can vary in strength depending on various factors. Research indicates that coastal afternoon winds can be strong, especially when influenced by sea breezes and specific geostrophic wind directions. The spatial variability of winds in coastal areas is significant, with local orography and sea breezes playing crucial roles in wind patterns. High-latitude sea breezes can lead to calm zones near the coast, while moderate large-scale flows can enhance coastal afternoon breezes. Bioindicators like wind-deformed trees can help assess mean wind speeds and directions in windy coastal regions, with the highest wind speeds typically felt near the shoreline. Therefore, while coastal winds can indeed be strong, their intensity is influenced by a combination of factors such as sea breezes, geostrophic wind direction, local topography, and proximity to the shoreline.
What are the different mechanisms that cause typhoon track deflection over taiwan topography?
10 answers
Typhoon track deflection over Taiwan's topography is influenced by several mechanisms, as revealed through various studies. The wavenumber 1 asymmetric structure plays a crucial role in the westward deflection of typhoons, where radar data assimilation helps in improving track forecast accuracy by analyzing this component. The topographic effects of the Central Mountain Range (CMR) significantly influence typhoon track deflection and intensity change, with the northward deflection being attributed to the strong flow induced to the east of the typhoon center in response to re-circulating flow around southern Taiwan. Lee vortices generated downstream of Taiwan's topography by steering flow and the interaction of the typhoon circulation with the topography lead to the development of TC-terrain-induced gyres, which play a part in the deflection process. The analysis of typhoons with deflection tracks near Taiwan shows that the northern landfall tropical cyclones experience significant cross-mountain flow, resulting in vorticity stretching and subsidence warming, which contribute to track deflection. The size of the tropical cyclone also affects the track deflection, with smaller TCs showing a more pronounced deflection due to the interaction with Taiwan's topography. Topographically-induced wavenumber-one flow with a pair of vorticity gyres around the typhoon center induces northward and then westward movement. The presence of the CMR influences cyclone circulation and associated track deflection, with simulations showing that removing the Taiwan terrain leads to more northward deflection earlier. Midtropospheric northerly asymmetric flow plays a leading role in causing southward deflection of simulated tropical cyclone tracks. Finally, the outer cyclonic flow at the western flank of a typhoon, when split around the northern part of the CMR, leads to strong convergence east of Taiwan, resulting in northward deflection. These studies collectively highlight the complex interplay of topographic effects, vortex-scale asymmetries, and environmental steering flows in influencing typhoon track deflection over Taiwan.
How pollutant concentration behave with traffic vehicles at first flush, peak flow and recession?
10 answers
The behavior of pollutant concentration in relation to traffic vehicles during different phases of stormwater runoff—first flush, peak flow, and recession—reveals complex dynamics influenced by various factors including traffic volume, weather conditions, and urban infrastructure. During the first flush, pollutants from roadway runoff are significantly concentrated, with the initial portion of runoff transporting a substantial mass of pollutants, indicating a pronounced first flush effect where the concentration of pollutants like Total Organic Carbon (TOC), heavy metals, and suspended solids sharply increases. This effect is attributed to the accumulation of pollutants on road surfaces during dry periods, which are then washed off by the initial stormwater, leading to higher concentrations. As the flow reaches its peak, the concentration of pollutants generally correlates well with traffic volume, suggesting that higher traffic flow rates contribute to increased pollutant loads. However, the relationship between traffic volume and pollutant concentration is not linear; during high flow rate events, the concentration of pollutants does not significantly increase, possibly due to the dilution effect as more stormwater is available to disperse the pollutants. During the recession phase, as the runoff volume decreases, the concentration of pollutants can either stabilize or decrease, depending on the pollutant type and the urban infrastructure's ability to manage and treat runoff. Studies have shown that the concentration of particulate pollutants in runoff fluctuates with rainfall intensity and can be impacted by the duration and depth of rainfall, indicating that the behavior of pollutants during the recession phase is also influenced by the characteristics of the rainfall event. Furthermore, the dispersion of pollutants in urban environments is affected by wind direction, speed, and urban street canyon effects, which can alter the distribution of pollutants during different runoff phases. The interaction between traffic-induced turbulence and environmental conditions, such as wind and thermal effects, plays a crucial role in determining the dispersion and dilution of pollutants in both the atmosphere and stormwater runoff. In summary, pollutant concentrations during the first flush are markedly higher due to the washing off of accumulated pollutants, peak flow concentrations are influenced by traffic volume and the dilution capacity of the runoff, and during recession, concentrations may decrease or stabilize, influenced by rainfall characteristics and urban infrastructure's effectiveness in runoff management.
Why are there drastic changes in wind movement in urban cities?
5 answers
Drastic changes in wind movement in urban cities occur due to various factors outlined in the research papers. The urban heat island effect, caused by concentrated structures and limited green cover, can lead to increased wind speeds in cities compared to rural areas, known as the urban wind island effect. Urban morphology, including building layout and relief, significantly alters wind speeds and directions within cities. Optimizing building structures can amplify wind flow, enhancing wind power generation potential in urban environments. High-rise buildings offer promising opportunities for decentralized electricity production through small-scale wind power, integrating sustainability into urban landscapes. These findings emphasize the importance of considering urban planning, building design, and local climate conditions to understand and harness wind movement effectively in urban areas.
Amihan season has strong winds
5 answers
During the amihan season, strong winds are observed in the Western Mediterranean Sea, particularly in the winter season, inducing surface cooling and anomalous ocean heat loss. In the Himalayan region near Mount Everest, strong afternoon winds are analyzed, with distinct wind patterns during the monsoon and non-monsoon seasons, driven by different atmospheric conditions. Additionally, forecasting peak wind speeds is challenging during the cool season, with tools developed to predict daily peak and average wind speeds based on various predictors, including synoptic weather patterns and inversion characteristics. These studies highlight the presence of strong winds during specific seasons and regions, emphasizing the variability and impact of intense wind events.
How does intense rainfall characteristic induce flood in nigeria?
5 answers
Intense rainfall characteristics induce floods in Nigeria by increasing the frequency and intensity of heavy rainfall events, leading to a higher risk of flooding. The heavy rainfall events are often triggered by factors such as high rainfall intensity, obstruction, siltation, and encroachment into flood-prone areas. These extreme rainfall events, exacerbated by issues like climate change, contribute significantly to flooding incidents, causing damage to properties and loss of human lives. Atmospheric conditions, such as strong moisture convergence and upward motion of convectively unstable moist air, play a crucial role in delivering heavy rainfall that results in flooding. Additionally, horizontal moisture flux divergence and convective available potential energy (CAPE) are key factors in forecasting extreme rainfall events, with moisture availability being a more significant contributor to higher rainfall amounts than wind shear.
What is Small Wind Turbines?
4 answers
Small wind turbines are compact devices designed to harness wind energy for electricity generation in areas with light to moderate wind speeds. Unlike large-scale wind turbines that produce megawatts of power, small wind turbines are cost-effective, require less space, and are suitable for residential use. These turbines convert wind's kinetic energy into mechanical energy, which is then transformed into electricity. Parameters like tip speed ratio and Reynolds number are crucial in maximizing power output and efficiency of small wind turbines. Recent advancements focus on optimizing blade design, airfoil selection, and generator efficiency for improved performance. Small wind turbines find applications in remote power systems, microgrids, and small desalination units, showcasing their versatility and potential for decentralized energy generation.
How Soil moisture contribute to factors promoting intense rainfall in nigeria?
5 answers
Soil moisture contributes significantly to factors promoting intense rainfall in Nigeria. Studies have shown that a pre-rainy season moisture build-up is crucial for abundant rainfall. Additionally, the horizontal moisture flux divergence (HMFD) plays a key role in forecasting extreme rainfall events, with values above 1.0 × 10−6 g kg−1 s−1 capable of producing substantial rainfall. Furthermore, the heavy rainfall event in Nigeria was linked to strong moisture convergence in the lower troposphere, indicating upward motion of convectively unstable moist air, which led to heavy precipitation. Moreover, the interactive effects of rainfall intensity and soil properties influence runoff generation, with alkalinity and rainfall intensity being key factors affecting runoff. Therefore, adequate soil moisture content is essential for creating the necessary atmospheric conditions that support intense rainfall events in Nigeria.
How land/sea thermal contrast contribute to factors promoting intense rainfall in nigeria?
5 answers
The land/sea thermal contrast plays a significant role in promoting intense rainfall in Nigeria by influencing various climatic factors. Studies have shown that the land/sea thermal gradient between selected locations in Nigeria and the tropical Atlantic Ocean affects rainfall onset and retreat dates. Additionally, the interaction between land surface temperature (LST) and sea surface temperature (SST) influences rainfall patterns in coastal zones, with higher SST and LST values correlating with increased rainfall. Furthermore, the modulation of diabatic heating associated with the land-sea thermal contrast affects the distribution of tropical cyclone (TC) activity energy sources and sinks, contributing to asymmetric TC activity distribution and intensity over oceans. The impact of land-sea contrast on rainfall asymmetry during tropical cyclone landfall is also evident, with rough land surfaces triggering more rainfall to the west.