Hurricanes.kennedy,jamie,grayson

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Hurricanes can form over warm ocean waters and spin due to wind. They have the potential to kill over a million people, as was the case during Hurricane Katrina in 2005. Hurricanes bring strong winds that can suck up objects and rip up grass, in addition to posing a serious threat to human life.

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BY :Kennedy, Jamie & Grayson! hurricanes! Kennedy,Jamie & grayson!

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Global warming is the observed century-scale rise in the average temperature of Earth's climate system.[2] Since 1971, 90% of the increased energy has been stored in the oceans, mostly in the 0 to 700m region.[3] Despite the oceans' dominant role in energy storage, the term "global warming" is also used to refer to increases in average temperature of the air and sea at Earth's surface.[4] Since the early 20th century, the global air and sea surface temperature has increased about 0.8 °C (1.4 °F), with about two-thirds of the increase occurring since 1980.[5] Each of the last three decades has been successively warmer at the Earth's surface than any preceding decade since 1850.

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RUNNING HEAD: Rough Draft-Peer review Page 1 PEER REVIEW Page 7 ROUGH DRAFT A few minutes of intense shaking, followed by a devastating tsunami, producing widespread destruction. FEMA's best-case scenario, 13,000 people will lose their lives, (Schultz, 2015). The question is not if it's going to happen, it's when. The countdown to catastrophe is on for the Pacific Northwest. We're talking about the Cascadia Subduction Zone. Throughout this paper, I will discuss the who, what, where, when, and how this overdue megaquake will strike. The Cascadia subduction zone is a 620-mile-long crack in the earth's crust. It is in the pacific northwest where the North American tectonic plate meets the Juan de Fuca plate, (Tarbuck, Lutgens, Tasa, 2017). Tectonic plates are pieces of crust that move across the earth's surface over millions of years, (Oskin, 2015). The subduction zone is where two tectonic plates meet. One eventually bends underneath the other, which is what we see in the North Pacific. The Juan de Fuca plate is sliding under the weaker, North American plate. Eventually, the North American plate will buckle, result in a devastating earthquake, followed by massive Tsunami. Subduction zones are found all along the edge of the Pacific in what is called, "The ring of fire." Off the coasts of Washington, Canada, Alaska, Russia, and Indonesia birthed the most devastating earthquakes, tsunamis and volcanic eruptions in history, (Oskin, 2015). The bigger the subduction zone, the higher magnitude of the earthquake. A subduction zone earthquake with a magnitude of 7.5 or greater will likely produce a tsunami. The Cascadia subduction zone is a big one. It runs 620 miles long and 62 miles wide. It has all the ingredients necessary to produce massive devastation. So how do we know that the Pacific Northwest is in danger? Tsunamis are a direct result of an earthquake, volcanic eruption or a massive landslide. The once dubbed, "Orphan Tsunami," hit the eastern coast of Japan on January 27th, 1700, (Atwater et al., 2015). The year 1700 in the Pacific Northwest was considered prehistory, meaning there were no written records of events. Japan, on the other hand, have produced numerous ancient writings of stories that told of flooded fields, wrecked houses, fire, a shipwreck, and evacuations. The Japanese knew that tsunamis were a result of an earthquake, and because they didn't feel any shaking prior, they called the event a high tide. At the time, it wasn't known that tsunamis could occur from earthquakes that happened from faraway lands. Outsiders of Northwestern North America scarcely knew of its existence. At that time, leading European geographers left that part of the map blank. So, for this mystery, the Japanese didn't even know the Pacific Northwest existed, much less that it had produced the earthquake that generated the tsunami, (Atwater et al., 2015). The Chilean earthquake that struck on May 22, 1960, generated a tsunami that surged a ...

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Caldeira, Ken. " The Great Climate Experiment ." Scientific American (2012): 78 -83. Academic Search Premier . Web. 1 Feb. 2013. Section: BEYOND LIMITS: WHERE WE'RE HEADED ECOLOGY How far can we push the planet? BUSINESS, GOVERNMENT OR TECHNOLOGY forecasts usually look five or 10 years out, 50 years at most. Among climate scientists, there is some talk of century's end. In reality, carbon dioxide dumped into the atmosphere today will affect Earth hundreds of thousands of years hence. How will greenhouse gases change the far future? No one can say for sure exactly how Earth will respond, but climate scientists -- using mathematical models built from knowledge of past climate systems, as well as the complex web of processes that impact climate and the laws of physics and chemistry -- can make predictions about what Earth will look like. Already we are witnessing the future envisioned by many of these models take shape. As predicted, there has been more warming over land than over the oceans, more at the poles than near the equator, more in winter than in summer and more at night than in the day. Extreme downpours have become more common. In the Arctic, ice and snow cover less area, and methane-rich permafrost soils are beginning to melt. Weather is getting weirder, with storms fueled by the additional heat. What are the ultimate limits of the change that we are causing? The best historical example comes from the 100-million-year-old climate of the Cretaceous period, when moist, hot air enveloped dinosaurs' leathery skin, crocodilelike creatures swam in the Arctic and teeming plant life flourished in the CO2-rich air. The greenhouse that is forming now will have consequences that last for hundreds of thousands of years or more. But first, it will profoundly affect much of life on the planet -- especially us. A DESERT IN ITALY ONE OF THE GREATEST uncertainties in climate prediction is the amount of CO2 that will ultimately be released into the atmosphere. In this article, I will assume industrial civilization will continue to do what it has been doing for the past 200 years -- namely, burn fossil fuels at an accelerating rate until we can no longer afford to pull them out of the ground. Just how much CO2 could we put into the atmosphere? All told, there are about one quadrillion metric tons (1021 grams) of organic carbon locked up in Earth's sedimentary shell in one form or another. So far we have burned only one twentieth of 1 percent of this carbon, or roughly 2,000 billion metric tons of CO2. With all the carbon locked in Earth's crust, we will never run out of fossil fuels. We are now extracting oil from tar sands and natural gas from water-fractured shale -- both resources once thought to be technologically and economically inaccessible. No one can confidently predict just how far ingenuity can take us. Yet eventually the cost of extraction and processing will become so high that fossil fuels will become more expensive than alternativ ...

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