Weather Makes a Difference: 8-hour
Ozone Trends for 1997-2007
State and Local Information for EPA Region 3
Maryland
Pennsylvania
Virginia
Washington, DC
West Virginia
Composite trend for available sites in these states:
EPA Region 03 (selected sites)
80
70
60 -
.Q
Q_
Q_
(D
C
o
N
o
8> 50
CD
> 40
<
c 30
o
CO
8 20
GO
8^--
8:
o..
Adjusted for Weather
• - * - U n adj u sted for Weath er
1998
2000
2002
Year
2004
2006
U.S. Environmental Protection Agency
Office of Air and Radiation
Office of Air Quality Planning and Standards
April 2008
-------
Maryland
Ozone
On average, ozone adjusted for weather conditions declined 10 percent between 1997 and
2007. These improvements in ozone are in response to both state and regional reductions
in NOx and VOC emissions. The level of ozone improvement varies from site to site.
Trends for 1997-2007 for rural sites and urban areas with complete ozone and
meteorology data are presented below. Ozone season (May 1 - September 30) averages
of daily maximum 8-hour ozone were adjusted to remove the influence of year-to-year
variability in weather conditions. The dotted line shows the trend in observed values at
monitoring sites, while the solid line illustrates the underlying ozone trend after removing
the effects of weather. The solid line serves as a m ore accurate ozone trend for assessing
changes in emissions. Typical weather conditions are determined by averaging
conditions (e.g., temperature, humidity, etc.) for the time period presented. The
information provided is useful for reviewing the weather influence for a particular ozone
season. The solid line represents ozone levels anticipated under typical weather
conditions.
Seasonal Average 8-hour Ozone Trends
Blackwater NWR, MD
.Q
Q.
CL
Q) 80
c
o
N
O
a> 60
O)
OS
L.
CD
- 40
03
C
o
co
TO
a) 20
CO
Adjusted for Weather
Unadjusted for Weather
. - o
O- ¦
. mesM ;j- - - o
--=-8-—
1998
2000
2002
Year
2004
2006
-------
Baltimore, MD 8-hr Ozone Trends
JQ
Q.
Cl
0 80
c
o
0
geo
e
1
S 40
c
o
$
" 20
o.
«
* *
$
Adjusted for Weather
Unadjusted for Weather
. - - O"
1998
2000
2002
Year
2004
2006
Beltsville, MD
JQ
CL
Q.
0 80
c
o
N
O
£.60
O)
03
L.
(D
- 40
co
C
O
if)
-------
Pennsylvania
Ozone
On average, ozone adjusted for weather conditions declined 12 percent between 1997 and
2007. These improvements in ozone are in response to both state and regional reductions
in NOx and VOC emissions. The level of ozone improvement varies from site to site.
Trends for 1997-2007 for rural sites and urban areas with complete ozone and
meteorology data are presented below. Ozone season (May 1 - September 30) averages
of daily maximum 8-hour ozone were adjusted to remove the influence of year-to-year
variability in weather conditions. The dotted line shows the trend in observed values at
monitoring sites, while the solid line illustrates the underlying ozone trend after removing
the effects of weather. The solid line serves as a m ore accurate ozone trend for assessing
changes in emissions. Typical weather conditions are determined by averaging
conditions (e.g., temperature, humidity, etc.) for the time period presented. The
information provided is useful for reviewing the weather influence for a particular ozone
season. The solid line represents ozone levels anticipated under typical weather
conditions.
Seasonal Average 8-hour Ozone Trends
Scranton, PA 8-hr Ozone Trends
rj
Ql
Q.
0 80
c
o
N
O
60
o>
CO
a>
5 40 H
to
c
o
-------
Allentown-Beth, PA 8-hr Ozone Trends
n
CL
Cl
0 80
c
o
N
0
a) 60
a»
co
0)
1 40
co
c
o
y)
ra
0) on
if) zu
. . o
i • * >
O-
V
Adjusted for Weather
Unadjusted for Weather
1998
2000
2002
Year
2004
2006
Arendtsville, PA
n
CL
Cl
CD
c
o
N
O
0) 60
D)
2
- 40 H
CO
c
o
tf)
co
0)
if)
20
Adjusted for Weather
Unadjusted for Weather
'V.
«*—— - o
© •**—
1998
2000
2002
Year
2004
2006
-------
Harrisburgh, PA 8-hr Ozone Trends
n
cl
CL
0) 80
c
o
N
O
(D 60
O)
CO
L.
0
- 40
CO
c
o
V)
CO
CD Of)
CO ZU
o o-"
Adjusted for Weather
Unadjusted for Weather
i i i
1998 2000 2002
i i
2004 2006
Year
Kane Exp. Forest, PA
£1
CL
Gl
0 80
c
o
N
o
oj 60
O)
CO
L.
0
f 40
CO
c
o
«/>
CO
0)
CO
Adjusted for Weather
Unadjusted for Weather
•—
o*'
-8_:
IS:
"o:
^S:
O.
20
1998
2000
2002
Year
2004
2006
-------
M.K, Goddard, PA
j2
Q.
CL
0) 80
c
o
N
O
^>60
D)
CO
i—
0
5 40
CO
-
o
to
CO
0) on
C/) zu
Adjusted for Weather
Unadjusted for Weather
o.
O,
.8^8=
O O'
S:
-•*
O-
1998
2000
2002
Year
2004
2006
Philadelphia, PA 8-hr Ozone Trends
jQ
Q.
CL
0 80
sz
o
N
0
® 60
O)
03
4_
0)
1 40
CO
c
o
U)
CIS
(1) on
05
o-'
"o-TTTS:
. o -
. a
-•
—- Adjusted for Weather
• - - - Unadjusted for Weather
1998
2000
2002
Year
2004
2006
-------
Pittsburgh, PA 8-hr Ozone Trends
n
Q_
Cl
CO
a)
40
ro
c
o
c/3
CO
0 90
CO zu
o - - - - o
*
—• —
o.
O-
o..
o*
—- Adjusted for Weather
¦ - - Unadjusted for Weather
1998
2000
2002
Year
2004
2006
-------
Virginia
Ozone
On average, ozone adjusted for weather conditions declined 14 percent between 1997 and
2007. These improvements in ozone are in response to both state and regional reductions
in NOx and VOC emissions. The level of ozone improvement varies from site to site.
Trends for 1997-2007 for rural sites and urban areas with complete ozone and
meteorology data are presented below. Ozone season (May 1 - September 30) averages
of daily maximum 8-hour ozone were adjusted to remove the influence of year-to-year
variability in weather conditions. The dotted line shows the trend in observed values at
monitoring sites, while the solid line illustrates the underlying ozone trend after removing
the effects of weather. The solid line serves as a m ore accurate ozone trend for assessing
changes in emissions. Typical weather conditions are determined by averaging
conditions (e.g., temperature, humidity, etc.) for the time period presented. The
information provided is useful for reviewing the weather influence for a particular ozone
season. The solid line represents ozone levels anticipated under typical weather
conditions.
Seasonal Average 8-hour Ozone Trends
Hortori Station, VA
JQ
CL
CL
0 80
c
o
N
o
a) 60
D)
CO
L.
-------
Prince Edward, VA
n
Q.
£L
0) 80
c
o
N
O
0 60
CD
<0
L.
CD
- 40
03
c
o
m
CO
0 90
CO zu
-—- Adjusted for Weather
Unadjusted for Weather
9>
o- *
«
o-
. - o
>#o
1998
2000
2002
Year
2004
2006
Richmond, VA 8-hr Ozone i rends
.Q
CL
Q.
80 -
-------
Roanoke, VA 8-hr Ozone Trends
.Q
Cl
£L
0 80
c
o
N
o
® 60
O)
CD
CD
5 40
03
sz
o
w
cs
0)
C/D
•o*
. o
o -
•rs
— o
20
Adjusted for Weather
Unadjusted for Weather
i i i
1998 2000 2002
i i
2004 2006
Year
Virginia Beach, VA 8-hr Ozone Trends
.o
CL
CL
a) 80
c
o
N
O
<3> 60
O)
CO
L.
CD
- 40
CO
c
o
C/5
CC
0)
CO
^8-
o.
-8—
20
Adjusted for Weather
Unadjusted for Weather
1998
2000
2002
Year
2004
2006
-------
Washington, DC
Ozone
In Washington, DC ozone adjusted for weather conditions declined 9 percent between
1997 and 2007. This improvement in ozone is in response to both state and regional
reductions in NOx and VOC emissions.
Trends for 1997-2007 for a site with complete ozone and meteorology data are presented
below. Ozone season (May 1 - September 30) averages of daily maximum 8-hour ozone
were adjusted to remove the influence of year-to-year variability in weather conditions.
The dotted line shows the trend in observed values at monitoring sites, while the solid
line illustrates the underlying ozone trend after removing the effects of weather. The
solid line serves as a more accurate ozone trend for assessing changes in emissions.
Typical weather conditions are determined by averaging conditions (e.g., temperature,
humidity, etc.) for the time period presented. The information provided is useful for
reviewing the weather influence for a particular ozone season. The solid line represents
ozone levels anticipated under typical weather conditions.
Seasonal Average 8-hour Ozone Trends
Washington, DC 8-hr Ozone Trends
.Q
CL
Q.
0 SO
c
o
N
o
a> 60
CTi
CO
L.
-------
West Virginia
Ozone
On average, ozone adjusted for weather conditions declined 12 percent between 1997 and
2007. These improvements in ozone are in response to both state and regional reductions
in NOx and VOC emissions. The level of ozone improvement varies from site to site.
Trends for 1997-2007 for rural sites and urban areas with complete ozone and
meteorology data are presented below. Ozone season (May 1 - September 30) averages
of daily maximum 8-hour ozone were adjusted to remove the influence of year-to-year
variability in weather conditions. The dotted line shows the trend in observed values at
monitoring sites, while the solid line illustrates the underlying ozone trend after removing
the effects of weather. The solid line serves as a m ore accurate ozone trend for assessing
changes in emissions. Typical weather conditions are determined by averaging
conditions (e.g., temperature, humidity, etc.) for the time period presented. The
information provided is useful for reviewing the weather influence for a particular ozone
season. The solid line represents ozone levels anticipated under typical weather
conditions.
Seasonal Average 8-hour Ozone Trends
Parsons, WV
JO
CL
Cl
0 80
a
o
N
o
S.60
O)
CO
L.
(D
- 40
CO
sz
o
CO
0) on
100 zu
Adjusted for Weather
Unadjusted for Weather
8rrrc8~8^.
1998
2000
2002
Year
2004
2006
-------
Cedar Creek, VW
n
Cl
CL
cd 80
c
o
N
O
Q) 60
O)
co
L.
60
O)
05
L.
-------
Huntington, WV 8-hr Ozone Trends
n
Cl
Cl
(u 80
c
o
N
O
60
O)
ro
©
- 40
CO
c:
o
------- |