Hazardous Substances in My Home? - Rivanna Regional Stormwater
Weather & Climate of Virginia - Rivanna Master Naturalists · Weather & Climate of Virginia Robert...
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Weather & Climate of Virginia
Robert E. Davis Professor of Climatology
Dept. of Environmental Sciences University of Virginia
Email: [email protected]
Rivanna Master Naturalists March 17, 2015
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Tropic of
Cancer
Arctic Circle
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SEASONS
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Effect of Solar Angle
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Radiation receipt: 1) sun angle (intensity) 2) day length (duration)
circle of illumination
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Top of Atmosphere Sunlight
Equator
Charlottesville
Arctic
34–36
0–44
16–41
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Continentality
Mean temperature of warmest minus coldest month
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Incoming
Outgoing
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General Circulation
of Atmosphere
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Ocean Circulation
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Jet Stream:
1) Boundary between warm, tropical and
cold, polar air masses
2) Size and strength vary seasonally
3) Linked to midlatitude
storms at surface
4) Linked to storm tracks
5) A component of
(circum)-polar vortex
cold
warm
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JULY
IN WINTER, JET STREAM 1) EXPANDS 2) STRENGTHENS
JANUARY
http://www.classzone.com/books/earth_science/terc/content/investigations/es1906/es1906page02.cfm
COLD! COOL
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A (Very) Short Course on Weather
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Storms are low pressure systems
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Types of Fronts
L
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Cold Front (vertical cross-section)
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Warm Front (vertical cross-section)
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Cold Air
Warm Air
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Average January Winds
Richmond
(color = speed)
North wind
Southwest wind
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Average July Winds
Richmond
(color = speed)
North wind
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July Mean Maximum Dew Point Temperature
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Common Wind Directions
Surface
Aloft
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Mountain Effects
(Elevation: 1000 feet)
(Elevation: 3500 feet)
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fronts
thunderstorms
hurricanes
Charlottesville Precipitation
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SUMMER
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% Rainfall (May-Nov) from Tropical Cyclones
Knight and Davis, 2007
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Charlottesville Climatic Water Budget
PE = Potential Evapotranspiration m
illim
eter
s
AE = Actual Evapotranspiration
P = Precipitation
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PE P
Surplus
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PE
P
Deficit
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PHENOLOGY
Study of cyclic and seasonal natural phenomena, especially in relation to climate and plant and animal life
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PHRENOLOGY
Study of the and size of the cranium as a (supposed) indication of
character and mental abilities
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Grape Phenology
Light, heat accumulation, soil moisture
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Organism Growth and Temperature
growth begins
growth at maximum
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Growing Degree Days (GDDs)
accumulated degrees over time above a baseline and below a maximum, based on daily mean temperature
April 10: Max = 65, Min = 45, so Mean = 55; 55 – 50 = 5 GDDs April 11: Max = 70, Min = 50, so Mean = 60; 60 – 50 = 10 GDDs
Season total = 15 GDDs
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Growing Degree Days (GDDs)
These vary by organism! corn baseline = 50°F
lettuce baseline = 42°F potato baseline = 46°F
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Growing Degree Days (GDDs)
As of Sunday (3/15), CHO had accumulated 44 (corn) GDDs—12 below
average for that date
Cautions Some organisms are more light than heat
sensitive, so GDDs will not be as useful
Proper growth depends on adequate soil
moisture as well as heat accumulation
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PLANT HARDINESS ZONES
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Average Date of Last Spring Frost
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Indicator LimitationsChanges in measurement techniques and instruments over time can affect trends. However, these data were carefully reviewed for quality, and values that appeared invalid were not included in the indicator. This indi-cator only includes weather stations that did not have many missing data points.
Data SourcesAll three figures are based on data compiled by the National Oceanic and Atmospheric Administration’s National Climatic Data Center, and these data are available online at: www.ncdc.noaa.gov/oa/ncdc.html. Trends were analyzed by Kunkel (2009).8
Length of Growing SeasonKey Points• The average length of the growing season in the lower 48 states has in-
creased by about two weeks since the beginning of the 20th century. A particularly large and steady increase occurred over the last 30 years (see Figure 1).
• The length of the growing season has increased more rapidly in the West than in the East. In the West, the length of the growing season has increased at an average rate of about 20 days per century since 1900, compared with a rate of about six days per century in the East (see Figure 2).
• The final spring frost is now occurring earlier than at any point since 1900, and the first fall frosts are arriving later. Since 1985, the last spring frost has arrived an average of about four days earlier than the long-term average, and the first fall frost has arrived about three days later (see Figure 3).
Figure 3. Timing of Last Spring Frost and First Fall Frost in the Lower 48 States, 1900–2002This figure shows the timing of the last spring frost and the first fall frost in the lower 48 states compared with a long-term average. Positive values indicate that the frost occurred later in the year, and negative values indicate that the frost occurred earlier in the year. The trend lines were smoothed using an 11-year moving average. Choosing a different long-term average for comparison would not change the shape of the trends.
Year
Devi
atio
n fro
m a
vera
ge (d
ays)
-6
-4
-2
0
2
4
6
Spring frost
Long-term average
Fall frost
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
Data source: Kunkel, 20097
61
(Kunkel, 2009)
Average Date of Last Spring and First Fall Frost Continental U.S.
Late
r E
arlie
r
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(Kunkel, 2009)
Length of Growing Season, 1900–2002 Continental U.S.
Length of Growing SeasonBackgroundThe length of the growing season in any given region represents the number of days when plant growth takes place. The growing season often determines which crops can be grown in an area, as some crops require long growing seasons, while others mature rapidly. Growing season length is limited by many different fac-tors. Depending on the region and the climate, the growing season is influenced by air temperatures, frost days, rainfall, or daylight hours.
Changes in the length of the growing season can have both positive and negative effects. Moderate warming can benefit crop and pasture yields in mid- to high-latitude regions, yet even slight warming decreases yields in seasonally dry and low-latitude regions.4 A longer growing season could allow farmers to diversify crops or have multiple harvests from the same plot. However, it could also limit the types of crops grown, encourage invasive species or weed growth, or strain water supplies. A longer growing season could also disrupt the function and structure of a region’s ecosystems, and could, for example, alter the range and types of animal species in the area.
About the IndicatorThis indicator looks at the length of the growing season in the lower 48 states, as well as trends in the timing of spring and fall frosts. For this indicator, the length of the growing season is defined as the period of time between the last frost of spring and the first frost of fall, when the air temperature drops below the freezing point of 32ºF.
Trends in the growing season were cal-culated using temperature data from 794 weather stations throughout the lower 48 states. These data were obtained from the National Oceanic and Atmospheric Administration’s National Climatic Data Center. Growing season length and the timing of spring and fall frosts were aver-aged spatially, then compared with a long-term average to determine the deviation from “normal” in any given year.
This indicator measures the length of the growing season in the lower 48 states.
Figure 1. Length of Growing Season in the Lower 48 States, 1900–2002This figure shows the length of the growing season in the lower 48 states compared with a long-term average. For each year, the line represents the number of days shorter or longer than average. The trend line was smoothed using an 11-year moving average. Choosing a different long-term average for comparison would not change the shape of the trend.
Year
-10
-5
0
5
10
15
Devi
atio
n fro
m a
vera
ge (d
ays)
Long-term average
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
Data source: Kunkel, 20095
Figure 2. Length of Growing Season in the Lower 48 States, 1900–2002: West Versus EastThis figure shows the length of the growing season in the western and eastern United States compared with a long-term average. The trend line was smoothed using an 11-year moving average. Choosing a different long-term average for comparison would not change the shape of the trends.
Year
Devi
atio
n fro
m a
vera
ge (d
ays)
-15
-10
-5
0
5
10
15
20
1900 1910 1920 1930 1940 1950 1960 1970 1980 1990 2000
West
East
Long-term average
Data source: Kunkel, 20096
60
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Weather & Climate of Virginia
Robert E. Davis Professor of Climatology
Dept. of Environmental Sciences University of Virginia
Email: [email protected]
Rivanna Master Naturalists March 17, 2015