Document ID: EPA-R01-OAR-2010-1043-0036
Agency: epa
Document Type: Supporting & Related Material
Title: 
Posted Date: 2011-11-30T05:00Z

TSD-1a

Meteorological Modeling using Penn State/NCAR 5th Generation Mesoscale
Model (MM5)

Bureau of Air Quality Analysis and Research

Division of Air Resources

New York State Department of Environmental Conservation

Albany, NY 12233

February 1, 2006

Meteorological Modeling using Penn State/NCAR 5th Generation Mesoscale
Model (MM5)

Version 3.6 of MM5 was used to generate annual 2002 meteorology for the
OTC modeling work. Prof. Dalin Zhang of the University of Maryland
performed the MM5 simulations in consultation with NYSDEC staff. The
model was applied in Lambert conformal map projection and utilized MPP
Version developed for clusters. The two-way nested domain consisted of
coarse (36km) and fine (12km) mesh corresponding to 149x129 and 175x175
grids, respectively, in this application (see Figure 1). 

 corner at (2340km, 1188km). In the vertical direction, the terrain
following σ-coordinate system was used with the pressure at each
σ-level determined from a reference state that is estimated using the
hydrostatic equation from a given sea-level pressure and temperature
with a standard lapse rate. There are 30 unevenly spaced σ levels,
giving 29 vertical layers, with higher resolution within the planetary
boundary layer (PBL).  The σ levels are:

1.0000, 0.9974, 0.9940, 0.8980, 0.9820, 0.9720, 0.9590, 0.9430, 0.9230,
0.8990,

0.8710, 0.8390, 0.8030, 0.7630, 0.7180, 0.6680, 0.6180, 0.5680, 0.5180,
0.4680,

0.3680, 0.3180, 0.2680, 0.2180, 0.1680, 0.1230, 0.0800, 0.0400, 0.0000

The surface layer was set at about 10m, the level at which surface winds
were typically observed, and the model top was set at 50hPa with a
radiative top boundary condition. The time steps for the 36km and 12km
domains were 75 and 25 seconds, respectively.

The important model physics options used for this MM5 simulation
include:

Kain-Fritsch (1993) convective scheme for both 36- and 12-km domains 

Explicit moisture scheme (without the mixed phase) containing prognostic
equations for cloud water (ice) and rainwater (snow) (Dudhia 1989; Zhang
1989)

Modified version of the Blackadar planetary boundary layer (PBL) scheme
(Zhang and Anthes 1982; Zhang and Zheng 2004)

Simple radiative cooling scheme (Grell et al. 1994)

Multi-layer soil model to predict land surface temperatures using the
surface energy budget equation (Dudhia 1996)

Note that the Blackadar PBL scheme has been modified in order to correct
the phase shift of surface wind speed and temperature diurnal cycle,
following a study that compared five different PBL schemes: the
Gayno-Seaman TKE scheme (Shafran et al. 2000), Burk-Thompson (1989),
Blackadar (Zhang and Anthes 1982), MRF (Hong and Pan 1996), and
Mellor-Yamada-Jajic (Mellor and Yamada 1974; Jajic 1990, 1994). The
details of the study can be found at Zhang and Zheng (2004).

Nudging Processes 

The MM5 provides options for nudging observations for each domain during
the model integration process (Stauffer and Seaman, 1990; Stauffer et
al. 1991). The Eta analyses of   upper-air winds, temperature and
water-vapor mixing ratio as well as their associated surface   fields
were used for nudging every 6 hours, and the Eta surface wind fields
blended with surface wind observations were used to nudge every 3 hours.
 While only the surface winds were nudged, their influences could extend
into the PBL as well (see Stauffer et al. 1991). Based on UMD’s prior
experience in numerical experiments, the following nudging coefficients
have been used: 

Upper-air wind fields: 5. 0E-4s-1 for Domain 1 (36km), and 2. 5E-4s-1
for Domain 2 (12km);  

Upper-air temperature fields: 1.0E-5s-1   for both Domains; 

Surface winds: 5. 0s-1E-4s-1 for Domain 1, and 2.5E-4s-1 for Domain 2;
and 

Surface temperature and moisture: not nudged due to instability
consideration. 

ASSESSMENT

This assessment covers the period of May through September 2002.

National Weather Service (NWS) and CASTNet data – Surface temperature,
Wind Speed, and Humidity

NWS (TDL) and CASTNet (  HYPERLINK "http://www.epa.gov/castnet/" 
www.epa.gov/castnet/ )surface measurements of temperature, wind speed,
and humidity (note there were no humidity measurements for CASTNet) were
used to compare with the MM5 outputs. The evaluation was performed with
METSTAT program developed by Environ Corporation
(www.camx.com/files/metstat.15feb05.tar.gz..When comparing to NWS data,
the METSTAT interpolates the first layer MM5 (at 10m height) temperature
and humidity data to a height of 2m, the level that corresponds to the
NWS measurement of these parameters. However, no such interpolation was
made for wind speed and direction. In the case of CASTNet surface
measurements, no such changes were needed as CASTNet data were reported
at a height of 10m. In this analysis, no exclusion was made for calm
conditions. The reported calm winds (zero wind speed measured) were
treated as is in this evaluation effort. The   METSTAT calculated
standard statistical measures – average, bias, error and index of
agreement between the measured and predicted parameters.

 Figure 2 displays the temperature and wind speed comparison of MM5 and
measured data from NWS and CASTNet networks for August 2002. MM5
performance for both in magnitude and diurnal timing, temperature can be
considered to be quite good for both NWS and CASTNet data, while MM5
underpredicted NWS and overpredicted CASTNet daytime wind speed,
respectively. It should be pointed out that there are differences in how
the meteorological information is collected and reported by the two
networks as well as in MM5. The CASTNet measurements are based on hourly
averaged wind speed while NWS reports 2min average at 10min before the
hour, whereas MM5 predictions are reflective of the last time-step of
the hour of computation. Interestingly, MM5 appears to track quite well
the nighttime minimum wind speed for both networks. In the case of
humidity (not shown), MM5 tracks the NWS observed humidity trend well,
but MM5 missed the observed semi-diurnal cycles.  Comparisons for the
five months including bias and root mean square error from both NWS and
CASTNet are available on request from NYSDEC. 

The above assessment is based on domain-wide averages to provide an
overall response of the model over the five months. Another way of
assessing the model is to examine the degree of correlation between the
measured and predicted parameters. Figure 3 displays such a comparison
for temperature and wind speed for the NWS hourly data covering the
period of May through September 2002. For the NWS data, the correlations
are in the range from 0.7 to 0.8 for wind speed, above 0.96 for
temperature, and in the range of 0.8 to 0.9 for humidity. CASTNet data
(not shown) also exhibit similar correlation. These correlations
indicate that MM5 simulation has captured both the diurnal and synoptic
scale variations. Detailed plots of this comparison are available on
request from NYSDEC.     

Vertical Profiler – Winds 

The Wind-Profiler network measurements along the U. S. East Coast
(www.madis-fsl.org/cap) were used to evaluate the vertical profiles from
MM5. There are twelve wind-profiler measurement stations from which data
were available for comparison. For convenience of comparison, the
wind-profiler measurements were interpolated to the MM5 vertical levels.
The approach used was simple interpolation between two adjacent
wind-profiler layers to the MM5 vertical level, and was limited to that
reported by the profiler measurement. The focus of the comparison was to
assess if MM5 was able to capture the measured vertical structure, and
for this we used the observed Low Level Jet (LLJ) as an indicator. The
comparison was performed for June, July and August 2002. In general it
is found that MM5 captures the profiler measured vertical wind field
structure reasonably well.  Figure 4 displays an example of the MM5 and
wind profiler comparison for the August 2002 episode at Richmond, VA and
Concord, NH. MM5 predicted weaker LLJ winds compared to those based on
the wind-profiler measurements. The detailed plots of this comparison
are available on request from NYSDEC.   

Cloud Cover – Satellite cloud image

Cloud information derived from satellite image data
(www.atmos.umd.edu/~srb/gcip/webgcip.htm )were used to assess the MM5
prediction of cloud cover. The 0.5o by 0.5o resolution of the satellite
data were interpolated into the 12km MM5 grid for comparison. The MM5
total cloud fraction was estimated by MCIP based on the MM5’s low
cloud, middle cloud and high cloud predictions. In general, MM5 captured
the satellite cloud pattern well but underestimates the satellite cloud
fraction (see Figure 5 as an example). Part of problem may due to the
coarse resolution of the satellite cloud data. The detailed plots of
this comparison are available on request from NYSDEC or at the following
URL     

Precipitation comparison

The monthly total observed precipitation data were constructed from
1/8-degree daily precipitation analysis data (  HYPERLINK
"http://data.eol.ucar.edu/codiac/dss/id=21.093" 
http://data.eol.ucar.edu/codiac/dss/id=21.093  produced by Climate
Prediction Center, based on 7,000-8,000 hourly/6-hourly gauge reports
and radar). The MM5 monthly total precipitation was estimated from the
MM5 predicted convective and non-convective rainfall and summed up for
each month. In general, MM5 captured the observed spatial patterns in
May and September, but no so well for June, July and August (See Figure
6), perhaps reflective of the summertime convective rain activities not
captured by MM5. Detailed plots of this comparison are available on
request from NYSDEC.   

Calm Conditions

Calm conditions are defined as observed wind speed of zero knots and
wind direction as 0o.  It would be useful to assess how MM5 performs
under observed calm conditions, because of potential pollutant buildup
that could occur under such conditions. Table 1 lists the summary of the
percentage of calm condition at each hour for the August 2002 from the
NWS data within the 12km domain. It is apparent from the Table that the
calm conditions occur primarily during the night and early morning
hours, from 23Z (7 p.m. EDT) to 15Z (11 a.m. EDT) with a peak at 10Z (6
a.m. EDT). To assess MM5 performance, the observed and MM5 predicted
wind speeds were divided into calm and non-calm according to observed
wind speed. Figure 7 displays such a comparison of the MM5 predicted
wind speed to the observed wind speed under the calm and non-calm
conditions for the month of August 2002. For the “calm” group, the
average wind speed for MM5 varies from 1 m/s during the night and early
morning hours and over 1.5 m/s during the day.  MM5 is over-predicting
during observed calm wind conditions.  There are local minima every 3
hours, due to the surface observed wind speed nudging in MM5. In
contrast under the non-calm conditions, MM5 underpredicts by about 0.5
m/s for all hours with noticeable local maximum happening at the nudging
hours. The MM5 nudging process would pull predictions toward the
measured data, while the underprediction of MM5 for the non-calm
conditions may due to the adopted PBL scheme in this simulation.

Summary

In this study, we performed an assessment of the MM5 simulation to
real-world data, both at the surface level as well as in the vertical.
While there are no specific recommended procedures identified for this
assessment, similar approaches have been   used elsewhere (Dolwick 2005,
Baker 2004, and Johnson 2004). Traditionally, the NWS surface
measurements are used for such a comparison. Since NWS data had been
used through nudging processes in developing the MM5 simulation, the
comparisons should not be far removed from each other. In this study, we
extended the evaluation by using CASTNet measurements that were not used
in the MM5 simulations. Thus comparison with CASTNet data provides for
an independent assessment and should complement the comparison with NWS
data. We also compared the MM5 results with the wind profiler data and
cloud data derived from satellite images to diagnose if the MM5
simulation is yielding the right type of dynamics in the vertical. The
analyses shows that in general, the performance of the MM5 is reasonable
both at the surface and in the vertical, thereby providing confidence in
the use of these data in the CMAQ simulations.

  

References 

Baker, K. 2004:   HYPERLINK
"http://www.ladco.org/tech/photo/photochemical.html" 
www.ladco.org/tech/photo/photochemical.html 

Burk, S. D. and W. T. Thompson, 1989:  A vertically nested regional
numerical weather prediction model with second-order closure physics.
Mon. Wea. Rev., 117, 2305–2324.  

Dudhia, J., 1989: Numerical study of convection observed during the
winter monsoon experiments using a mesoscale two-dimensional model. J.
Atmos. Sci., 46, 3077–3107. 

Dudhia, J., 1996: A multi-layer soil temperature model for MM5.
Preprints, 6th Annual MM5 Users Workshop, Boulder, CO.

Dolwick, P. 2005:   HYPERLINK
"http://cleanairinfo.com/modelingworkshop/presentations/MPE_Dolwick.pdf"
 http://cleanairinfo.com/modelingworkshop/presentations/MPE_Dolwick.pdf 

Grell, G. A., J. Dudhia , and D. R. Stauffer 1994:  A description of the
fifth-generation Penn State/NCAR Mesoscale Model (MM5). NCAR Tech.Note
NCAR/TN-398 1 STR, 122 pp. 

Hong, S.-H., and H.-L. Pan, 1996: Nonlocal boundary layer vertical
diffusion in a medium-range forecast model. Mon. Wea. Rev., 124,
2322–2339. 

Jajic, Z.  I., 1990: The step-mountain coordinate: Physical package. 
Mon. Wea. Rev., 118, 1429-1443. 

Jajic, Z. I., 1994: The step-mountain Eta coordinate model: Further
development of the convection, viscous sublayer and turbulent closure
schemes. Mon. Wea. Rev., 122, 927-945.

Johnson, M. 2004:   HYPERLINK
"http://www.ladco.org/tech/photo/photochemical.html" 
www.ladco.org/tech/photo/photochemical.html 

Kain, J.S., and J.M. Fritsch, 1993:  Convective parameterization for
mesoscale models: The Kain-Fritsch scheme. Cumulus Parameterization.
Meteor. Monogr., 46,  Amer.  Meteor. Soc., 165-170. 

Mellor, G.  L., and T. Yamada, 1974:  A hierarchy of turbulence closure
models for planetary boundary layers. J. Atmos. Sci., 31, 1791–1806. 

Shafran,  P.C.,  N.L.  Seaman, and G. A.  Gayno, 2000: Evaluation of
numerical   predictions of boundary layer structure during the Lake
Michigan ozone study.  J.  Appl.  Meteor.,  39,  412-426. 

Stauffer, D. R., N. L. Seaman and F. S. Binkowski 1991:  Use of
four-dimensional data assimilation in a limited-area mesoscale model.
Part II: Effects of data assimilation within the planetary boundary
layer. Mon. Wea. Rev., 119, 734-754. 

Stauffer, D.  R. and N. L. Seaman, 1990:  Use of four-dimensional data
assimilation in a limited-area mesoscale model.  Part I:  Experiments
with synoptic-scale data. Mon.  Wea.  Rev.,  118, 1250-1277. 

Zhang, D.-L.,  1989:  The  effect  of  parameterized  ice  microphysics 
on  the  simulation  of  vortex circulation with a mesoscale hydrostatic
model. Tellus, 41A, 132-147. 

Zhang, D.-L,  and  R. A. Anthes,  1982:  A high-resolution  model  of 
the  planetary  boundary  layer-sensitivity tests and comparisons with
SESAME-79 data. J. Appl. Meteor., 21, 1594–1609. 

Zhang, D.-L, and W.-Z.  Zheng, 2004: Diurnal cycles of surface winds and
temperatures as simulated by five boundary-layer parameterizations. J.
Appl. Meteor., 43, 157-169. 

Table 1 	Measured calm and non-calm occurrences over the modeling domain
during August 2002 based on NWS data

Hour	#Non-Calm	#Calm	#Total	% Calm

00Z	18209	3924	22133	17.7

01Z	16531	6026	22557	26.7

02Z	15604	6929	22533	30.8

03Z	14983	7245	22228	32.6

04Z	14309	7540	21849	34.5

05z	14073	7735	21808	35.5

06Z	13934	7949	21883	36.3

07Z	13792	8040	21832	36.8

08Z	13542	8273	21815	37.9

09Z	13542	8385	21927	38.2

10Z	13708	8591	22299	38.5

11Z	14139	8693	22832	38.1

12Z	15297	7690	22987	33.5

13Z	17336	5192	22528	23

14Z	18522	3439	21961	15.7

15Z	18755	2617	21372	12.2

16Z	19169	2015	21184	9.5

17Z	19555	1617	21172	7.6

18Z	19982	1430	21412	6.7

19Z	20149	1389	21538	6.4

20Z	20565	1288	21853	5.9

21Z	20518	1383	21901	6.3

22Z	20672	1556	22228	7

23Z	20231	2292	22523	10.2



Figure 1: OTC MM5 modeling domain with areal extent of 12km and 36km
grids

Figure 2:  Temperature and Wind speed comparisons for August 2002. In
each case the upper panel corresponds to comparison between MM5 and NWS
data and the lower panel between MM5 and CASTNet data.

 

Figure 3a:	Spatial correlation estimates between MM5 and NWS data for
wind speed

                         from May to September 2002

 

Figure 3b:  	Spatial distribution of correlation coefficients for
Temperature between                                        MM5 and NWS
data from May to September 2002.

Richmond, VA

 

 

Concord, NH

 

 

›

›

œ

☊଀െጀ撤᐀撤㜀$␸䠀$⑛封Ĥ

ጀ撤᐀撤㜀$␸䠀$⑛封ĤĀ਀&䘋

愀Ĥ²欀兤

9pper and lower panes at each station are for MM5 and profiler,
respectively. The abcissa represents day and the ordinate the height
(m).

 

 

Figure 5: MM5 and Satellite cloud images for August 14, 2002 at 0700 EST

 

 

Figure 6: MM5 predicted and measured precipitation over the domain for
the month of August 2002 

 

Figure 7: Comparison of averaged wind speed between MM5 and observed
under calm (C) and non-calm (NC) conditions.

 PAGE   

 PAGE   1