The Into The Storm !!HOT!!

In the town of Silverton, Oklahoma, the local high school senior class is preparing for graduation. The high school's vice-principal, Gary Fuller, has asked his two sons, Trey and Donnie, to record messages from the seniors for a time capsule to be opened in 25 years. Elsewhere, Pete, a veteran storm chaser, has been attempting to intercept and film tornadoes using a Tornado Intercept Vehicle nicknamed Titus, but has come up short all year long. Upon learning of a major line of developing storms, the chasers decide to head for Silverton in hopes of filming tornadoes. After arriving in Silverton, the team discovers that the cell they had been chasing has dissipated, but the Silverton cell abruptly strengthens, resulting in a hailstorm and tornado. As the team films, the funnel shifts course and heads for the high school.

At the high school, the weather suddenly sours. The students are marshaled into the school building. In the aftermath of the tornado, shaken students emerge from the damaged building to view the destruction, while Gary sets out to rescue his eldest son Donnie, who had gone to an abandoned paper mill to help his friend Kaitlyn with a project; both were subsequently trapped when the tornado brought the building down on them.

The Into The Storm

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As Pete's storm chase team stops in a small part of town, a tornado takes shape just as Gary and Trey arrive, destroying several buildings. Before the tornado dissipates Gary must save Pete's meteorologist, Allison Stone. Then, Pete's team agree to help Gary get to the paper mill. While en route, another round of tornadoes form and encircle Pete's team, in the process destroying a residential neighborhood and a car lot. An explosion turns one of the tornadoes into a firenado, which Jacob the cameraman tries to film, only to be caught up in the storm and killed. This causes friction in the team, as Pete's concern seems to be more on collecting data than ensuring his team's safety. After recovering their vehicles, Allison leaves with Gary to continue their trip to the paper mill.

In the skies above Silverton, a convergence of two large tornadoes results in a colossal EF-5 tornado that threatens to level the town. The town's citizens have taken shelter at the school, but Pete's team determines that the school's storm shelter will be inadequate. Unable to alert the school's staff with mobile devices, Pete's team rushes to the school. While citizens rush to board school buses, Pete and his team follow the storm, but the last school bus and a handful of cars are cut off from the retreat due to a downed transmission tower.

The storm chasers and school refugees take cover in a storm drain at a construction site, but a truck from the airport that the tornado struck damages one of the storm grates, compromising the shelter. In an attempt to save lives, Pete hands over his research hard drives to Gary, then sacrifices himself by leaving the shelter to move Titus down to the storm grate, to use the vehicle to anchor the storm grate to the concrete face and has the others tie its towline to the crashed truck for support. Titus's equipment proves unable to anchor the vehicle to the ground, and the tornado picks up the vehicle. From the camera turret aboard Titus, Pete observes the funnel of the tornado as the vehicle is lifted above the clouds, fulfilling his dream, before then crashing to the ground, killing him and wrecking Titus. Shortly thereafter, the EF-5 tornado dissipates.

The cytokine storm has captured the attention of the public and the scientific community alike, and while the general notion of an excessive or uncontrolled release of proinflammatory cytokines is well known, the concept of a cytokine storm and the biological consequences of cytokine overproduction are not clearly defined. Cytokine storms are associated with a wide variety of infectious and noninfectious diseases. The term was popularized largely in the context of avian H5N1 influenza virus infection, bringing the term into popular media. In this review, we focus on the cytokine storm in the context of virus infection, and we highlight how high-throughput genomic methods are revealing the importance of the kinetics of cytokine gene expression and the remarkable degree of redundancy and overlap in cytokine signaling. We also address evidence for and against the role of the cytokine storm in the pathology of clinical and infectious disease and discuss why it has been so difficult to use knowledge of the cytokine storm and immunomodulatory therapies to improve the clinical outcomes for patients with severe acute infections.

On August 23rd, a tropical depression formed over the southeastern Bahamas, becoming Tropical Storm Katrina on August 24th as it moved into the central Bahamas. The storm continued to track west while gradually intensifying and made its initial landfall along the southeast Florida coast on August 25th as a Category 1 hurricane (80mph) on the Saffir-Simpson Hurricane Scale. After moving west across south Florida and into the very warm waters of the Gulf of Mexico, Katrina intensified rapidly and attained Category 5 status (with peak sustained winds of 175mph) for a period of time as it moved northwest on August 28th. Katrina weakened to a Category 3 before making landfall along the northern Gulf Coast, first in southeast Louisiana (sustained winds: 125mph) and then made landfall once more along the Mississippi Gulf Coast (sustained winds: 120mph). Katrina finally weakened below hurricane intensity late on August 29th over east central Mississippi.

The damage and loss of life inflicted by this massive hurricane in Louisiana and Mississippi was staggering with significant effects extending into Alabama and the western Florida panhandle. This was a storm that captivated the public and media with most coverage occurring in the New Orleans area. Considering the scope of its impacts, Katrina was one of the most devastating natural disasters in United States history.

As Katrina set new minimum central pressure records while approaching the northern Gulf Coast on Sunday, August 28th, the storm made its final turn to the north as it moved toward southeastern Louisiana. Katrina was a large storm with a very distinct eye. Early on the 28th, Katrina reached a minimum central pressure of 902mb (at the peak) - ranking 7th lowest on record for all Atlantic Basin hurricanes - and rapidly intensified to a Category 5 (175mph).

In this velocity loop (759-859am CDT), the eye of the storm, denoted by the large white circle, is southwest of the region of maximum surface wind speeds. These measurements are the winds flowing toward KMOB radar. [Color scale where the next highest velocity values begin: gray = 104mph; brown = 109mph; dark blue = 114mph; cyan = 117mph; green >127 mph]

The Saffir-Simpson Hurricane Wind Scale is a 1 to 5 rating based only on a hurricane's maximum sustained wind speed. This scale does not take into account other potentially deadly hazards such as storm surge, rainfall flooding, and tornadoes.

The Saffir-Simpson Hurricane Wind Scale estimates potential property damage. While all hurricanes produce life-threatening winds, hurricanes rated Category 3 and higher are known as major hurricanes*. Major hurricanes can cause devastating to catastrophic wind damage and significant loss of life simply due to the strength of their winds. Hurricanes of all categories can produce deadly storm surge, rain-induced floods, and tornadoes. These hazards require people to take protective action, including evacuating from areas vulnerable to storm surge.

*In the western North Pacific, the term "super typhoon" is used for tropical cyclones with sustained winds exceeding 150 mph.

Storm water is defined by US EPA as the runoff generated when precipitation from rain and snowmelt events flows over land or impervious surfaces without percolating into the ground. Storm water is often considered a nuisance because it mobilizes pollutants such as motor oil and trash. In most cases, storm water flows directly to water bodies through sewer systems, contributing a major source of pollution to rivers, lakes, and the ocean. Storm water discharges in California are regulated through National Pollutant Discharge Elimination System (NPDES) permits. However, storm water may also act as a resource and recharge to groundwater when properly managed. The Water Boards are actively involved in initiatives to improve the management of storm water as a resource. For more information read our Storm Water Management Fact Sheet

The Federal Clean Water Act (Clean Water Act) prohibits certain discharges of storm water containing pollutants except in compliance with a National Pollutant Discharge Elimination System (NPDES) permit. The NPDES stormwater program regulates some stormwater discharges from three potential sources: municipal separate storm sewer systems (MS4s), construction activities, and industrial activities.

STORMS' mission is to lead the evolution of storm water management in California by advancing the perspective that storm water is a valuable resource, supporting policies for collaborative watershed-level storm water management and pollution prevention, removing obstacles to funding, developing resources, and integrating regulatory and non-regulatory interests.

The mission of the Storm Water Grant Program is to promote the beneficial use of storm water and dry weather runoff in California by providing financial assistance to eligible applicants for projects that provide multiple benefits while improving water quality.

The Water Boards are working toward innovative storm water quality solutions including incorporation of low impact development objectives, green chemistry pollutant control, and education outreach through films.

Scientists aboard the aircraft deploy Global Positioning System (GPS) dropwindsondes as NOAA Corps officers pilot and navigate the P-3 through the hurricane. These instruments continuously transmit measurements of pressure, humidity, temperature, and wind direction and speed as they fall toward the sea, providing a detailed look at the structure of the storm and its intensity. The P-3s' tail Doppler radar and lower fuselage radar systems, meanwhile, scan the storm vertically and horizontally, giving scientists and forecasters a real-time look at the storm. The P-3s can also deploy probes called bathythermographs that measure the temperature of the sea. be457b7860