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Benjamin McKeown

This year's El Nino will be the strongest in 18 years, WMO says - Technology & Science ... - 0 views

  • The current El Nino weather phenomenon is expected to peak between October and January and could turn into one of the strongest on record, experts from the World Meteorological Organization said at a news conference on Tuesday.
  • waters in the east-central Pacific Ocean are likely to be more than 2 degrees hotter than average,
  • Arctic warming effect at work on the Atlantic jetstream current.
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  • "The truth is we don't know what will happen. Will the two patterns reinforce each other? Will they cancel each other? Are they going to act in sequence? Are they going to be regional? We really don't know,"
  • it is still unclear how global warming is affected by the frequency or magnitude of El Nino events.
Benjamin McKeown

Global warming 'will make our winters colder' - Climate Change - Environment - The Inde... - 0 views

  • Climate scientists believe they have found evidence to suggest that the loss of floating Arctic sea ice in the Barents and Kara seas north of Scandinavia can affect the global circulation of air currents and lead to bitterly cold winds blowing for extended periods in winter over Central Asia and Europe, including the UK.
  • the cooling effect is unlikely to last beyond this century
  • Rising global temperatures will eventually cancel out any localised cooling caused by loss of Arctic sea ice, although they said it is not possible to predict when this will happen.
Benjamin McKeown

Tropical Cyclones - 0 views

  • In the western Pacific they are called typhoons, and in the southern hemisphere they are called cyclones.  But, no matter where they occur they represent the same process.
  • Tropical cyclones are dangerous because of their high winds, the storm surge produced as they approach a coast, and the severe thunderstorms associated with them. Although death due to hurricanes has decreased in recent years due to better methods of forecasting and establishment of early warning systems, the economic damage from hurricanes has increased as more and more development takes place along coastlines.
  • Warm ocean waters (of at least 26.5°C [80°F]) throughout about the upper 50 m of the tropical ocean must be present.  The heat in these warm waters is necessary to fuel the tropical cyclone. The atmosphere must cool fast enough with height, such that it is potentially unstable to moist convection. It is the thunderstorm activity which allows the heat stored in the ocean waters to be liberated and used for tropical cyclone development. The mid-troposphere (5 km [3 mi] altitude), must contain enough moisture to sustain the thunderstorms. Dry mid levels are not conducive to the continuing development of widespread thunderstorm activity. The disturbance must occur at a minimum distance of at least 500 km [300 mi] from the equator. For tropical cyclonic storms to occur, there is a requirement that the Coriolis force must be present.  Remember that the Coriolis effect is zero near the equator and increases to the north and south of the equator.  Without the Coriolis force, the low pressure of the disturbance cannot be maintained.
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  • There must be a pre-existing near-surface disturbance that shows convergence of moist air and is beginning to rotate. Tropical cyclones cannot be generated spontaneously. They require a weakly organized system that begins to spin and has low level inflow of moist air. There must be low values (less than about 10 m/s [20 mph]) of vertical wind shear between the surface and the upper troposphere. Vertical wind shear is the rate of change of wind velocity with altitude.  Large values of vertical wind shear disrupt the incipient tropical cyclone by removing the rising moist air too quickly, preventing the development of the tropical cyclone. Or, if a tropical cyclone has already formed, large vertical shear can weaken or destroy it by interfering with the organization around the cyclone center.
  • unstable atmosphere
  • his instability increases the likelihood of convection, which leads to strong updrafts that lift the air and moisture upwards, creating an environment favorable for the development of high, towering clouds.
  • Surface convergence (indicated by the small horizontal arrows in the diagram below) causes rising motion around a surface cyclone (labeled as "L"). The air cools as it rises (vertical arrows) and condensation occurs.  The condensation of water vapor to liquid water releases the latent heat of condensation into the atmosphere. This heating causes the air to expand, forcing the air to diverge at the upper levels (horizontal arrows at cloud tops).
  • Since pressure is a measure of the weight of the air above an area, removal of air at the upper levels subsequently reduces pressure at the surface. A further reduction in surface pressure leads to increasing convergence (due to an higher pressure gradient), which further intensifies the rising motion, latent heat release, and so on. As long as favorable conditions exist, this process continues to build upon itself
  • When cyclonic circulation begins around the central low pressure area, and wind speeds reach 62 km/hr (39 mi/hr) the disturbance is considered a tropical storm and is given a name.  When wind speeds reach 119 km/hr (74 mi/hr) it becomes a hurricane.
Benjamin McKeown

Looming megadroughts in western US would make current drought look minor | Environment ... - 0 views

  • California is in its sixth year of drought, which was barely dented by rains brought by the El Niño climate event and sparked a range of water restrictions in the state. But warming temperatures and uncertain rainfall mean that if more isn’t done to slow climate change, droughts lasting 35 years are likely to blight western states by the end of the century, according to the study, published in Science Advances.
  • Such a megadrought would impose “unprecedented stress on the limited water resources”
  • the study predicts a 70% chance of a megadrought by the end of the century,
Benjamin McKeown

Blaming natural disasters on climate change will backfire. - 0 views

  • Thus, the migration in response to the severe and prolonged drought exacerbated a number of the factors often cited as contributing to the unrest, which include unemployment, corruption, and rampant inequality. The conflict literature supports the idea that rapid demographic change encourages instability. Whether it was a primary or substantial factor is impossible to know, but drought can lead to devastating consequences when coupled with preexisting acute vulnerability, caused by poor policies and unsustainable land use practices in Syria’s case and perpetuated by the slow and ineffective response of the Assad regime [emphasis added].
  • suggests that an unprecedented drought accentuated frustration with the Assad regime and led to migration from rural to urban areas.
  • While climate change will probably increase the number and intensity of heavy showers, leading to more frequent landslides, intensive logging and government negligence in permitting new construction in these areas cause the real disasters.
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  • While global warming probably accentuated the torrential rains, it was actually policy failures that allowed heavy rains to cause the flood and human suffering: Over the past two decades, the city government has systematically disregarded basic principles of ecology and urban planning by building structures in flood plains and marshlands.
  • Climate change is often going to be the domino that falls. But that does not mean we can ignore the rest of the dominos in the row.
Benjamin McKeown

Frozen conflict | The Economist - 0 views

  • IN 2007 a Russian-led polar expedition, descending through the icy waters of the Arctic Ocean in a Mir submarine, planted a titanium Russian tricolour on the sea bed 4km (2.5 miles) beneath the North Pole. “The Arctic has always been Russian,
  • Denmark has staked a claim to the North Pole, too. On December 15th it said that, under the UN Convention on the Law of the Sea (UNCLOS), some 900,000 square kilometres of the Arctic Ocean north of Greenland belongs to it (Greenland is a self-governing part of Denmark).
  • Canada, which plans to assert sovereignty over part of the polar continental shelf (
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  • he prize for these countries is the mineral wealth of the Arctic, which global warming may make more accessible.
  • an eighth of the world’s untapped oil
  • perhaps a quarter of its gas.
  • Drilling for oil and gas there is extremely expensive, and falling oil prices have made the economics of Arctic energy even less favourable. This gives would-be prospectors an interest in co-operating, not in adding to the risks and costs.
  • The melting of the summer sea ice has also opened up trade routes between Asia and Europe via the top of the world; 71 cargo ships plied the north-east passage last summer, up from 46 in 2012
  • Russia
  • carried out extensive combat exercises in the Arctic for the first time since the end of the cold war
  • re-equipping old Soviet bases there and in July tested the first of its new-generation rockets,
  • Sweden spent part of the summer searching for a Russian submarine that it suspected of slipping into its territorial waters.
  • countries may control an area of seabed if they can show it is an extension of their continental shelf.
Benjamin McKeown

Rising Seas - Interactive: If All The Ice Melted - 0 views

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Benjamin McKeown

Greenhouse Gases - 0 views

  • As a measure of this efficiency, greenhouse gases are often assigned a value for "Global Warming Potential" (GWP). This value is simply a comparison of the efficiency of a gas relative to CO2 over a time span of 100 years. Therefore a gas with a GWP of 20 is 20 times more efficient at retaining heat than CO2 over a 100 year time period.
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    Water has a GWP of 0.23
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