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    Changes in Extreme Precipitation in the Northeast United States: 1979–2014

    Source: Journal of Hydrometeorology:;2019:;volume 020:;issue 004::page 673
    Author:
    Howarth, Macy E.
    ,
    Thorncroft, Christopher D.
    ,
    Bosart, Lance F.
    DOI: 10.1175/JHM-D-18-0155.1
    Publisher: American Meteorological Society
    Abstract: AbstractExtreme precipitation can have significant adverse impacts on infrastructure and property, human health, and local economies. This paper examines recent changes in extreme precipitation in the northeast United States. Daily station data from 58 stations missing less than 5% of days for the years 1979?2014 from the U.S. Historical Climatology Network were used to analyze extreme precipitation, defined as the top 1% of days with precipitation. A statistically significant (95% confidence level) increasing trend of the threshold for the top 1% of extreme precipitation events was found (0.3 mm yr?1). This increasing trend was due to both an increase in the frequency of extreme events and the magnitude of extreme events. Rainfall events ≥ 150 mm (24-h accumulation) increased in frequency from 6 events between 1979 and 1996 to 25 events between 1997 and 2014, a 317% increase. The annual daily maximum precipitation, or the highest recorded precipitation amount in a given year, increased by an average of 1.6 mm yr?1, a total increase of 58.0 mm. Decreasing trends in extreme precipitation were observed east of Lake Erie during the warm season. Increasing trends in extreme precipitation were most robust during the fall months of September, October, and November, and particularly at locations further inland. The analysis showed that increases in events that were tropical in nature, or associated with tropical moisture, led to the observed increase in extreme precipitation during the fall months.
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      Changes in Extreme Precipitation in the Northeast United States: 1979–2014

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    contributor authorHowarth, Macy E.
    contributor authorThorncroft, Christopher D.
    contributor authorBosart, Lance F.
    date accessioned2019-10-05T06:49:01Z
    date available2019-10-05T06:49:01Z
    date copyright3/8/2019 12:00:00 AM
    date issued2019
    identifier otherJHM-D-18-0155.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263507
    description abstractAbstractExtreme precipitation can have significant adverse impacts on infrastructure and property, human health, and local economies. This paper examines recent changes in extreme precipitation in the northeast United States. Daily station data from 58 stations missing less than 5% of days for the years 1979?2014 from the U.S. Historical Climatology Network were used to analyze extreme precipitation, defined as the top 1% of days with precipitation. A statistically significant (95% confidence level) increasing trend of the threshold for the top 1% of extreme precipitation events was found (0.3 mm yr?1). This increasing trend was due to both an increase in the frequency of extreme events and the magnitude of extreme events. Rainfall events ≥ 150 mm (24-h accumulation) increased in frequency from 6 events between 1979 and 1996 to 25 events between 1997 and 2014, a 317% increase. The annual daily maximum precipitation, or the highest recorded precipitation amount in a given year, increased by an average of 1.6 mm yr?1, a total increase of 58.0 mm. Decreasing trends in extreme precipitation were observed east of Lake Erie during the warm season. Increasing trends in extreme precipitation were most robust during the fall months of September, October, and November, and particularly at locations further inland. The analysis showed that increases in events that were tropical in nature, or associated with tropical moisture, led to the observed increase in extreme precipitation during the fall months.
    publisherAmerican Meteorological Society
    titleChanges in Extreme Precipitation in the Northeast United States: 1979–2014
    typeJournal Paper
    journal volume20
    journal issue4
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-18-0155.1
    journal fristpage673
    journal lastpage689
    treeJournal of Hydrometeorology:;2019:;volume 020:;issue 004
    contenttypeFulltext
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