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Twentieth century trends in dew point temperature throughout the Upper Midwest

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Twentieth century trends in dew point temperature throughout the Upper Midwest Jesse Wartman Mentors: Daryl Herzmann and Dr. Eugene Takle Why are dew-point ... – PowerPoint PPT presentation

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Title: Twentieth century trends in dew point temperature throughout the Upper Midwest


1
Twentieth century trends in dew point temperature
throughout the Upper Midwest
  • Jesse Wartman

Mentors Daryl Herzmann and Dr. Eugene Takle
2
Why are dew-point temperatures important?
  • Important in forecasting
  • Used for specific and relative humidities
  • Regulate transpiration and evaporation processes
  • Key factors in the surface energy and
    hydrological budgets
  • Water vapor is the strongest contribution to the
    greenhouse effect

3
Past Studies
  • Gaffen and Ross (1999)
  • Increase through spring and fall
  • Robinson (1998)
  • Dew points were lower in the Upper Midwest during
    the winter
  • Robinson (2000)
  • Increase of 0.9F per 100 years over U.S.
  • Increase over spring and fall

4
Possible Errors
  • Non-uniform stations
  • Technology and instrument changes
  • 1950s - sling psychrometers
  • 1960s dial hygrothermometers
  • Most recent HO-83 dial hygrothermometer (NWS)

5
Hypotheses
  • Dew-point temperatures have experienced
    significant, positive trends over the past 44
    years in the Upper Midwest.
  • Those dew-point temperature tendencies are no
    different from trends that have been found across
    the rest of the United States in past studies.

6
Data and Methods
  • Hourly obs through IEM from the NCDC
  • 1961-2005
  • Monthly
  • Seasonal
  • Winter - December, January, February
  • Spring - March, April May
  • Summer - June, July August
  • Fall - September, October, November
  • Yearly
  • Decadal

7
Observation Stations
  • Legend of Cities
  • St. Louis
  • Kansas City
  • Omaha
  • Des Moines
  • Sioux Falls
  • Minneapolis

8
Missing Data
  • Sioux Falls 0
  • Minneapolis 18 - data gap decadal averages
    were substituted in, no significant change so
    left out
  • Omaha 30.11 - no data before 1974
  • Des Moines 1.33 - data gap
  • Kansas City 27.27 - no data before 1973
  • St. Louis 27.27 - no data before 1973

9
Significance
  • Significant if P-value lt 0.05
  • Semi-significant if P-value lt 0.1
  • P-Value calculated in JMP, observed
    significance probability from t-ratios
  • T-ratio tests hypothesis that each parameter is
    zero, ratio of the parameter estimate to its
    standard error

10
  • RESULTS
  • Monthly Climatic Trends
  • Seasonal climatic trends
  • Yearly average climatic trends
  • Decadal climatic trends
  • Twenty-two year climatic trends
  • Extreme days
  • Precipitable water

11
Monthly Climatic TrendsP-Value lt 0.05 P-value
lt 0.1
12
Seasonal Climatic Trends
Td (F)
13
Seasonal Climatic Trends
Td (F)
14
Seasonal Climatic Trends
Td (F)
15
Seasonal Climatic Trends
Td (F)
16
Yearly Average Climatic Trends
Td (F)
17
Yearly Climatic Trends
  • Averages
  • Kansas City .128
  • Sioux Falls .1
  • Minneapolis .083
  • Des Moines .077
  • Omaha .064
  • St. Louis .0084
  • Total 7.54F per 100 years
  • 0.9F per 100 years (Robinson, 2000)

18
Decadal Climatic Trends
Td (F)
Td (F)
19
Decadal Climatic Trends
Td (F)
Td (F)
20
Twenty-two year trends
  • 1961-1983
  • Omaha -64F
  • St. Louis -13F
  • Des Moines -5 F
  • Minneapolis -4F
  • Kansas City -3F
  • Sioux Falls 4F
  • 1984-2005
  • Omaha 12F
  • St. Louis 13F
  • Des Moines 11F
  • Minneapolis 13F
  • Kansas City 14F
  • Sioux Falls 11F

21
Twenty-two year trends
22
Pacific Decadal Oscillation (PDO)
23
Extreme days dew points over 70F
24
Extreme days dew points over 75F
25
Precipitable Water
  • Surface Vapor Pressure
  • Po 1mbe 1.81(17.27D)/(D237.3)
  • Precipitable Water
  • h Po /(?wg)

26
Precipitable Water
27
Implications
28
Implications
  • Precipitation
  • Heat stress
  • Crop production
  • Soil errosion
  • Water supplies
  • Human health
  • Heat waves

29
Concluding Remarks
  • Shift from negative trend to positive trend
  • Positive overall trend
  • Hypotheses
  • Dew-point temperatures have experienced
    significant, positive trends over the past 44
    years in the Upper Midwest. -gt TRUE
  • Those dew-point temperature tendencies are no
    different from trends that have been found across
    the rest of the United States in past studies. -gt
    FALSE
  • 7.54F over 100 years in Upper Midwest
  • 0.9F over 100 years in United States

30
Future Work
  • Modelling studies
  • Future increases?
  • Increase in greenhouse gases
  • PDO
  • El Niño
  • Atlantic Oscillation
  • Other factors

31
Acknowledgements
  • Daryl E. Herzmann
  • Eugene S. Takle
  • Jon Hobbs

32
Questions?
  • jwartman_at_iastate.edu
  • http//www.meteor.iastate.edu/jwartman/portfolio/
    project.html
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