APPENDIX C. TYPICAL METEOROLOGICAL YEAR (TMY2) ASSIGNMENTS

TABLE OF CONTENTS

C.1 INTRODUCTION

.......................................................................................................... C­1

C.1.1 Purpose and Intent.................................................................................................. C­1

C.1.2 Issues...................................................................................................................... C­1

C.2 APPROACH

................................................................................................................... C­1

C.2.1 Additional Data Sets

.............................................................................................. C­1

C.2.2 Mapping Approach

................................................................................................ C­4

C.2.3 Calculating State­by­State Weighting Factors....................................................... C­7

LIST OF FIGURES

Figure C.2.1 Locations of TMY2 Stations Superimposed on Heating Degree­Day Contours.. C­2

Figure C.2.2 Locations of 4775 NOAA Stations....................................................................... C­3

Figure C.2.3 Locations of Populated Places (PPL).................................................................... C­3

Figure C.2.4 PPL→NOAA Mappings for Iowa Showing a Predominance of Nearest­Location

Mappings.......................................................................................................... C­5

Figure C.2.5 PPL→NOAA Mappings for Washington Showing Some Distant Mappings in

Mountainous Regions

...................................................................................... C­5

Figure C.2.6 NOAA→TMY2 Mappings

................................................................................... C­7

C­iAPPENDIX C. TYPICAL METEOROLOGICAL YEAR (TMY2) ASSIGNMENTS

C.1 INTRODUCTION

C.1.1 Purpose and Intent

This appendix describes the methodology by which weighting factors were developed to

scale the influence of each TMY2 weather station on each state's results. The intent is to ensure

that the cost­effectiveness calculations properly reflect the geographic distribution of buildings in

which the HVAC systems under analysis will be used. State­level aggregate results need to be

most heavily influenced by the climates having the most buildings.

C.1.2 Issues

TMY2 stations, of which there are 239 in the United States, are distributed throughout the

country so as to give good coverage of the climatic variation in the United States. Unfortunately

for this study, the TMY2 stations are not distributed so as to match the distribution of buildings.

It is therefore necessary to identify a reasonable mapping between the climate­based (TMY2)

simulation results and the geographical distribution of buildings in each state. Although TMY2

data give good climatic coverage, they do not give sufficient geographical coverage.

Detailed data on the geographical/climatic distribution of buildings were not readily

available for this task. However, data on the geographical distribution of persons (population

data) can serve as a reasonable surrogate for buildings data, and are available from a number of

sources. The problem facing this study was to match up population data, which are available in

great geographical detail but not matched to climate indicators, with TMY2 data, which

characterize climate quite well but are not connected to any population indicators.

C.2 APPROACH

Figure C.2.1 shows the locations of the 239 TMY2 stations superimposed on a contour

map showing heating degree­days (HDD). It is clear that the geographic distribution of the

TMY2 stations is too sparse to capture many of the climate variations that occur over relatively

short distances, especially in mountainous regions. It is therefore not feasible to develop

weighting factors based solely on the TMY2 stations within a state.

C.2.1 Additional Data Sets

To develop weighting factors, we identified two data sets (in addition to the TMY2 data

set) that provide a connection between detailed population distribution and TMY2 stations.

These are:

• NOAA Climate Stations

– The National Climatic Data Center's (NCDC)'s “CLIM81”

database contains summary statistics from a large number of climate stations in the United

States. We used the 1961–1990 period of record (POR), which corresponds to the POR used

to define the TMY2 weather tapes, for which 4775 climate stations are represented (see

http://lwf.ncdc.noaa.gov/oa/documentlibrary/clim81supp3/clim81.html ). Each NOAA

station is characterized by its location (latitude/longitude), annual heating and cooling

degree­days, elevation, and various other metrics.

C­1Figure C.2.1 Locations of TMY2 Stations Superimposed on Heating Degree­Day Contours

• USGS Populated Places

– The United States Geological Survey (USGS), in its Geographic

Names Information System, maintains a detailed database of cities, towns, and other

important features. (For the latest version of this data set, see

http://geonames.usgs.gov/stategaz/00README.html

. Our analysis used a version of this

data set from the early 1990s, making it contemporaneous with the TMY2 and NOAA data

sets.) Of interest to this task are the PPL features known as “populated places,” which are

generally cities and towns, but also include large housing subdivisions, trailer parks, and

other places where people may live. For many of these populated places, the USGS has a

population estimate. The populated places (PPL) data give excellent geographical coverage.

The version of the data set used here has over 22,000 entries that include a population

1 estimate out of more than 164,000 total. Each PPL location is characterized by its location

(latitude/longitude), elevation, population, and various other metrics.

The NOAA data are important because they contain climate summary information that

can be mapped to the TMY2 stations, greatly increasing our geographical coverage.

Figure C.2.2 shows the locations of the 4775 NOAA stations. The PPL database is used to make

the final link between the climate information in the mapped NOAA/TMY2 stations and the

geographical distribution of population. Figure C.2.3 shows the PPL locations.

Locations without USGS population estimates tend to be those with very little population. We have kept these

smaller sites in our mapping analysis by assigning each a population estimate of one. This gives them

negligible influence against the more populous locations but allows the mapping procedure to work even in very

sparsely populated regions of some states.

C­2 1Figure C.2.2 Locations of 4775 NOAA Stations

Figure C.2.3 Locations of Populated Places (PPL)

C­3C.2.2 Mapping Approach

Our approach to generating TMY2 weighting factors involves three major steps:

1. Map each PPL location in the United States to a best­representative NOAA station. This

gives each location some summary climate metrics (chiefly, heating and cooling degreedays) that facilitate further mapping.

2. Map each NOAA station to a best­representative TMY2 station. This completes the link

between the geographic population estimates (PPL data) and the TMY2 stations.

3. For each state, compute the fraction of the total PPL population that “points” (via its

PPL→NOAA→TMY2 mappings) to each TMY2 station.

These are described in order below.

C.2.2.1 Mapping Populated Places Locations to NOAA Stations

Mapping each of the 164,000+ PPL locations to a best­representative NOAA station is a

mostly straightforward process. Because there is no climate information in the PPL database, the

only metrics available to associate each PPL location with a NOAA station are location

(latitude/longitude) and elevation (although elevation is not known for all PPL locations). The

mapping algorithm is as follows.

1. For each PPL location, identify the nearest NOAA station. Distances between

PPL/NOAA pairs are calculated using the latitudes and longitudes of the two locations

and simple spherical geometry. If the elevation of the nearest NOAA station is within

300 feet of the PPL location or if the elevation of the PPL location is unknown, then the

nearest NOAA station is the final mapping.

2. If the nearest NOAA station differs in elevation from the PPL location by more than

300 feet:

a) Identify the 20 closest NOAA stations to the PPL location.

b) Choose, from among the 20, the NOAA station that is nearest in elevation to the PPL

location.

This algorithm is imperfect in many situations, but was designed by trial and error to give

reasonable mappings in a large majority of cases. In locations with relatively flat terrain and

fairly dense population, the algorithm almost always maps to the closest NOAA station.

Figure C.2.4 shows the mappings in the state of Iowa as an example. Each plotted point on the

graphic is one NOAA station; the “hairs” are drawn outward to the various PPL locations

mapped to that station. In mountainous terrain or in locations with large distances between PPL

locations (e.g., Alaska), the second part of the algorithm does a reasonable job of identifying a

representative NOAA station, even if that station is some distance from the PPL location.

Figure C.2.5 shows the mappings for Washington as an example. Note that many of the PPL

locations (the ends of the hairs) are mapped to distant NOAA stations.

C­4Figure C.2.4 PPL→NOAA Mappings for Iowa Showing a Predominance of NearestLocation Mappings

Figure C.2.5 PPL→NOAA Mappings for Washington Showing Some Distant Mappings in

Mountainous Regions

C­5C.2.2.2 Mapping NOAA Stations to TMY2 Stations

Having mapped each PPL location to a best­representative NOAA station, the next step is

to map each NOAA station to a best representative TMY2 station. Because the NOAA and

TMY2 data sets provide less dense geographical coverage and because both data sets contain

climate information, this mapping process relies less on spatial proximity and more on similarity

of climate. Proximity remains important, though. In finding a best TMY2 mapping for a NOAA

station, we hope for similarity in a number of climate variables: temperature (HDD and CDD),

solar and wind characteristics, rainfall and humidity characteristics, snowfall, etc. The NOAA

data set supports direct comparison only of heating and cooling degree­days, but we rely on

spatial proximity to ensure similarity in the other variables.

The NOAA­to­TMY2 mapping algorithm is as follows.

1. For each NOAA station, identify the nearest TMY2 station. If the elevation of the

nearest TMY2 station is within 300 feet of the NOAA station, then the nearest TMY2

station is the final mapping.

2. If the nearest TMY2 station differs in elevation from the NOAA station by more than

300 feet, then select instead the TMY2 station that has the minimum “combined distance”

from the NOAA station. The combined distance is defined as the sum of the literal

distance (miles) between the two stations and an “equivalent latitude miles” value that

accounts for known differences in heating and cooling degree­days and elevation. This

latter metric requires some explanation (see below).

The equivalent latitude miles metric was developed as a means to characterize

temperature (HDD and CDD) and elevation in the same units as literal distance (i.e., miles). By

casting HDD, CDD, and elevation effects into units of miles, we are able to simply sum the

literal distance between two locations with the equivalent HDD/CDD/elevation distance to give

the two values equal weight in assigning a best­representative TMY2 station to each NOAA

station.

The equivalent latitude miles values are based on several related observations. First,

differences in both heating and cooling degree­days correlate with differences in latitude.

Second, those same degree­day differences also correlate with differences in elevation.

Combining these observations, we discovered that differences in north­south distances

(i.e., latitude miles) can be characterized in terms of differences in HDD, CDD, and elevation.

That is, as one moves northward (increasing latitude) and upward (increasing elevation), HDD

tends to increase and CDD tends to decrease. A regression analysis of these correlations allows

us to cast HDD, CDD, and elevation differences into units of distance (miles). A linear

regression on NOAA/TMY2 station pairs within 300 miles of each other gives the following

result.

d

= I + α × Δ HDD + β × CDD + γ × Δ Elev Eq. 7.1

equiv

where

d

equiv = equivalent latitude distance (miles),

Δ

HDD

= difference in heating degree­days (base­65F)

Δ CDD

= difference in cooling degree­days (base­65F)

C­6Δ Elev

= difference in elevation (feet)

I

= ­6.8938

α = 0.1061

β

= ­0.0149

γ = ­0.0718

The best representative TMY2 station for each NOAA station was selected as the one

with the minimum sum of actual distance and equivalent latitude distance. Figure C.2.6 shows

the final NOAA→TMY2 mappings for the continental United States. Each plotted point is a

TMY2 station, from which lines are drawn outward to the NOAA stations mapped to it.

Figure C.2.6 NOAA→TMY2 Mappings

C.2.3 Calculating State­by­State Weighting Factors

Weighting factors were developed for each U.S. state that express the fraction of that

state’s population that is represented by each TMY2 station. These weighting factors are based

directly on the PPL→NOAA→TMY2 mappings described above. The weighting factor for a

TMY2 station is defined as the summed population of all PPL locations in the state that point to

that TMY2 station divided by the summed population of all PPL locations in the state. Thus, the

sum of all the TMY2 weighting factors for a state is 1.0.

C­7