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    Systematic Biases in Manual Observations of Daily Maximum and Minimum Temperature

    Source: Journal of Climate:;1994:;volume( 007 ):;issue: 005::page 834
    Author:
    Nese, Jon M.
    DOI: 10.1175/1520-0442(1994)007<0834:SBIMOO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The authors demonstrate that manual observations of daily maximum and minimum temperature are strongly biased toward temperatures ending in certain digits. The nature and severity of these biases are quantified using standard statistical methods. Temperatures ending in ?0?, ?2?, ?5?, and ?8? are overrepresented in the data, with the bias toward multiples of ten being most statistically significant. Inconsistencies in the distribution of the data by final digit suggest that biasing toward a temperature T may result not only from misobservations of temperatures T ± 1 but also from misobservations of temperatures T ± 2. Although changes adopted by the U.S. Weather Bureau in 1950 in the rules governing the rounding of temperature observations improved several of the biases, all biases remained statistically significant after the rule revision. To estimate the potential effect of these biases on the mean and standard deviation of a temperature distribution, biasing simulations were performed on various normal distributions. In addition, it is shown that these biases can affect other relevant climatic statistics, such as the number of days that certain temperature thresholds are reached.
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      Systematic Biases in Manual Observations of Daily Maximum and Minimum Temperature

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4180512
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    contributor authorNese, Jon M.
    date accessioned2017-06-09T15:22:23Z
    date available2017-06-09T15:22:23Z
    date copyright1994/05/01
    date issued1994
    identifier issn0894-8755
    identifier otherams-4190.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4180512
    description abstractThe authors demonstrate that manual observations of daily maximum and minimum temperature are strongly biased toward temperatures ending in certain digits. The nature and severity of these biases are quantified using standard statistical methods. Temperatures ending in ?0?, ?2?, ?5?, and ?8? are overrepresented in the data, with the bias toward multiples of ten being most statistically significant. Inconsistencies in the distribution of the data by final digit suggest that biasing toward a temperature T may result not only from misobservations of temperatures T ± 1 but also from misobservations of temperatures T ± 2. Although changes adopted by the U.S. Weather Bureau in 1950 in the rules governing the rounding of temperature observations improved several of the biases, all biases remained statistically significant after the rule revision. To estimate the potential effect of these biases on the mean and standard deviation of a temperature distribution, biasing simulations were performed on various normal distributions. In addition, it is shown that these biases can affect other relevant climatic statistics, such as the number of days that certain temperature thresholds are reached.
    publisherAmerican Meteorological Society
    titleSystematic Biases in Manual Observations of Daily Maximum and Minimum Temperature
    typeJournal Paper
    journal volume7
    journal issue5
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1994)007<0834:SBIMOO>2.0.CO;2
    journal fristpage834
    journal lastpage842
    treeJournal of Climate:;1994:;volume( 007 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian