Current Events

  • Irish Chronicles Document Links Between Volcanoes and Weather
    A study of over 40,000 written entries in Irish Annals and ice core measurements shows a strong corr...Read more

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    Irish Chronicles Document Links Between Volcanoes and Weather

    A study of over 40,000 written entries in Irish Annals and ice core measurements shows a strong correlation between the occurrence of volcanic eruptions and extreme cold weather in Ireland over a 1200 year period. Data analyzed in this study cover the period from 431 to 1649, during which time up to 48 volcanic eruptions are identified in Greenland ice core records through deposition of volcanic sulfate in annual layers of ice. You can find the study (open access), published on 6 June 2013 in IOP Publishing's journal Environmental Research Letters, at http://iopscience.iop.org/1748-9326/8/2/024035/article. Find out more about how volcanoes can influence climate.
  • EF-5 Tornado in El Reno, Oklahoma Widest Ever Recorded in US
    The EF-5 tornado that hit El Reno, Oklahoma on May 31st was the widest ever recorded in the US, acco...Read more

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    EF-5 Tornado in El Reno, Oklahoma Widest Ever Recorded in US

    The EF-5 tornado that hit El Reno, Oklahoma on May 31st was the widest ever recorded in the US, according to the National Weather Service in Norman Oklahoma. The tornado, which remained on the ground for 40 minutes and reached 2.6 miles across (4.2 km), took the lives of 18 people including storm chasers Tim Samaras, Paul Samaras and Carl Young. For more information on the tornado, visit http://ow.ly/i/2hfDG.
  • Atmospheric CO2 Level Tops 400 ppm
    During the week of May 13th, the CO2 level at the Mauna Loa Observatory in Hawaii topped 400 ppm rep...Read more

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    Atmospheric CO2 Level Tops 400 ppm

    During the week of May 13th, the CO2 level at the Mauna Loa Observatory in Hawaii topped 400 ppm repeatedly. Daily levels of CO2 can vary due to weather, and there are seasonal trends as well. The level of atmospheric greenhouse gases continues to increase, now over 120 ppm since the Industrial Revolution began. For more on the Keeling Curve, see http://keelingcurve.ucsd.edu/. Find out more about greenhouse gases and warming.
This photo shows what happens to a landscape after an ice storm of freezing rain. The storm happened in Corning, KS on December 10-11, 2007.
Click on image for full size
National Weather Service Forecast Office of Topeka, KS

Sleet and Freezing Rain

Sleet forms when a partially melted snowflake or raindrop turns back into ice as it is falling through the air. Sleet starts out in the clouds as a snowflake or a raindrop. If it starts out as a snowflake, this means the layer it starts out in has a below freezing temperature; if it starts out as a raindrop then the first layer has an above freezing temperature. As the snowflake or raindrop falls towards the ground, it then moves through a warmer above freezing layer. This layer causes the snowflake to start to melt. Next the raindrop and the melted snowflake travel through a colder layer which is below freezing; this last layer causes the raindrop to freeze and the melted snowflake to refreeze. Sleet is usually tiny clear ice pellets that bounce when they hit the ground. An ice pellet is about 0.2 inches (5mm) or less, which is smaller than hail.

Freezing Rain happens when raindrops fall in liquid form and immediately freeze as they hit a cold surface. The process for freezing rain is similar to the process for sleet, except that freezing rain goes through a deeper layer of above freezing temperatures, allowing the snowflake to melt even further. The last layer the raindrop and melted snowflake travel through is rather small, unlike the last layer sleet travels through. This small layer causes the raindrops to become extremely cold. In this case, the ground level will have been below freezing for at least few hours if not several days. Freezing drizzle is similar to freezing rain but is much smaller and always starts out as a raindrop.

Freezing rain causes highways or roadways to be like ice skating rinks for automobiles. Since freezing rain freezes on contact with a surface, over time the amount of ice on an object increases. This can cause extensive damage to trees and power lines because the weight of the ice is too heavy for these objects. In January 1998 an ice storm or freezing rain storm hit northern New England and Canada and left millions of people without power in their homes.


Last modified July 24, 2008 by Vanessa Pearce.

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