
Frequently Asked Questions and Help
Weather
Warehouse (WxW) Overview
The goal behind the WxW was to assemble the most
comprehensive and robust database of historical and real-time weather
observations and to make these data available to users in a convenient
and affordable way.
In total the WxW databases
contain weather information from ten of
thousands of weather stations with histories in some cases extending
back over 100 years. The datasets which comprise the WxW database
originate from numerous government and non-government sources. The
collection of original datasets are rigorously quality controlled by
Weather Source and merged together to create a
“super” database of weather information that is
more accurate and more complete than the any of the original datasets.
From the WxW database Weather Source then produces a suite of weather
data products to fit a broad range of user needs. The hourly and daily
WxW products are listed in the following table. A glossary of terms for these
products may be found here.
| Daily Weather Products | Hourly Weather Products |
| Daily
Basic Daily
High Temperature Daily Low Temperature Daily Mean Temperature Daily Total Rainfall Daily Total Snowfall HDD (Heating Degree Days) CDD (Cooling Degree Days) GDD (Growing Degree Days) | Hourly Basic Temperature Precipitation Cloud Cover Wind Speed and Direction Dew Point Humidity Visibility Significant Weather Observations (Rain, freezing rain, snow, fog, thunder, lightning, hail, tornado) |
Data Densities
Weather stations don't supply perfect weather data.
Many stations have
been around for decades, but some are defunct and no longer report,
while others are new and only recently began reporting. Regardless, it
is common for stations to occasionally miss reports. This can be
because a station was temporarily off-line, there was an error in
transmission or because government agencies do not always supply all
station data.
In order to help you find the best data for your
search, we
analyze each station's data to quantify the completeness and present
this to you with your search results. We call the completeness the Data
Density.
The higher the data density, the better. We provide the data density
for each product. Ideally you would like to have data that is 100%
complete for the time period you are requesting, but
this is not always possible. Using the data densities, you can find the
station with the
most complete set of data for your search results. We provide density
information for all stations that were active at any point during the
time period you are interested in. If you cannot find a station with a
high enough data density, try broadening your search to a wider radius
using the Smart Search feature. If you are interested in a particular
day, narrow your search to that one day. Note that, for example, if you
are looking for only temperature information and the data density for
temperature is 100%, it won't matter to you if the data density for
snow is not 100%.
Some stations may not be in operation for the entire range of your request. The listing "Available period" will tell you whether the station was working during the period you have requested. The fact that the station was working does not mean that data for all dates will be there (see above), but this will let you know if the station was not even returning data during part of the period of your request. If the station was not in operation at the beginning or end of your requested period, we will only provide (and charge you for) the date range when the station was operational.
Just because a station may not have 100% complete data does not mean it will not be suitable for your needs. If, for example, you are looking for temperatures and snow data is missing, the data would still be good for your uses.
| - Data Availability: expand to determine suitability |
| Data Completeness: Hi Temp = 99.73% Lo Temp = 99.73% Precipitation = 99.73% Snow = Not Available
|
In the example we see that the station will report virtually all temperature and precipitation, but there is no data for snow. Use this information as a guide in choosing a station, remembering that you will be able to see exactly what data is missing ont he Final Review and Purchase page.
On the station selection page, each station provides additional information. Open this information by clicking on the "+" symbol. There is informatoin on the station itself and also the data densities. Where it says: Data Density: expand to determine suitability you can get a general idea of what data is being reported by the station. It is also possible to obtain exact information on the station via the Data Availability Map.
The Data Availability Map is a visual representation of all data points within the station's operational time frame. You can quickly look at any date available and see whether there is data present before paying for it. The data map is displayed on the Final Review and Payment page. If no station is suitable we suggest that you go back and enlarge the search area so that you may find another station, perhaps farther away, but which suits your needs.
Credit
Card Verification Value Code Location The Card Verification Value Code (CVV) is a number used to help prevent fraud in credit card transactions where the card is not present (such as phone or internet orders). | |
American Express ![]() The 4 digit number is on the front right or left of the card | Visa, Mastercard ![]() The number is on the back of the card, the last 3 digits on the signature line. |
There
are many types of weather stations which report data compiled by the US
Government. Some may be automated stations that report back
"in
real time", others may be manned by real human beings who typically
record their observations for the
previous 24 hours each morning, usually 7am. Thus, for example if it
rained on Oct. 26, the observerwould not report the amount in
his
rain guage until 7am on the 27th, and this amount would go down into
the books for the 27th.
The same thing might apply to snow. For this reason if you
are
interested in a specific day, it might be a good idea to "bracket" that
day with a day or so on either side.
Glossary of Weather Parameters
Cooling Degree Days is an index used by the power industry to
reflect the need for power for cooling or air conditioning.
CDD are determined by the equations and logic as follows:
Avg_Temp(F)
= (Max_Temp(F) + Min_Temp(F)) / 2.0
If Avg_Temp(F)
is greater than 65F, Then
CDD =
Avg_Temp(F) – 65
Else
CDD = 0
CDD positive example:
If on a given day a weather station records a minimum temperature of
60F and a maximum of 90F, then:
75(F) = (90F + 60F)
/ 2.0
If 75F is greater than 65F then
CDD = 75 – 65 = 10
CDD zero example:
If
on a given day a weather station records a minimum temperature of
50F and a maximum of 70F, then:
60(F) = (70(F) +
50(F)) / 2.0
If 60(F) is greater than 65F then
CDD = Avg_Temp(F) – 65
Else
CDD = 0
CDD are computed for each day
where maximum and
minimum temperatures are recorded. CDD are often summed over a month or
season. For example if a weather station averages 10 CDD per day, it
is not uncommon to hear statement such as: “The weather
station in New York City reported a total of 300 CDD for the month of
June”
Cloud
Cover
Cloud Cover is the amount of sky that
is filled with clouds. Weather
Source provides Cloud Cover in terms of percent, for example a Cloud
Cover observation of 75% means that 75% of the sky is filled with
clouds.
Dew Point
Dew Point
Temperature is the temperature to which air must be cooled in
order for saturation to occur. At this temperature, water vapor in the
air can condense to form dew on surfaces in contact with the air. The
Dew Point temperature is measure and/or derived at constant air
pressure and constant water vapor content.
Feels
Like Temperature
Feels Like
Temperature is a derived temperature index that merges wind
chill, regular temperature and heat index into a single
“Feels Like Temperature” index. Feels Like
Temperature is a convenient way to represent what the temperature feels
like to people in a single parameter.
GDD (Growing Degree Days)
Growing
Degree Days are calculated in a similar fashion to Cooling
Degree Days, except the threshold is set to 50F as opposed to 65F in
the Cooling Degree Day calculation. The purpose of GDDs is to estimate
how much energy crops have received. The maturity of many crops can be
estimated by the number of GDD that accumulate from the point in time
that they where planted. For example many varieties of corn generally
ready for harvest after a period of time in which 1100 to 1200 GDD have
occurred. The use of 50F as the threshold for Growing Degrees Days is
the most commonly used threshold, however other thresholds are often
used for specific crops. For example a threshold of 41F is often used
for Alpha crops. The GDD provide by Weather Source is based on a
threshold of 50.
HDD
(Heating Degree Days)
Heating
Degree Days is an index used by the power industry to reflect
the need for energy in producing heat for buildings. HDD are
essentially the opposite of CDD and are determined by the equations and
logic as follows:
Avg_Temp(F)
= (Max_Temp(F) + Min_Temp(F)) / 2.0
If Avg_Temp(F) is less
than 65F, Then
HDD = 65 -
Avg_Temp(F)
Else
HDD = 0
HDD positive example:
If
on a given day a weather station records a minimum temperature of
35F and a maximum of 55F, then:
45(F) = (55F + 35F)
/ 2.0
If 45F is less than 65F then
HDD = 65 – 45 = 20
HDD zero example:
If on a given day a weather station records a minimum temperature of 60F and a maximum of 80F, then:
70(F) = (80(F) + 60(F)) / 2.0
If 70(F) is
less than 65F then
CDD = 65F -
Avg_Temp(F)
Else
CDD = 0
HDD are computed for each day
where maximum and
minimum temperatures are recorded. HDD are often summed over a month or
season. For example if a weather station averages 10 HDD per day, it
is not uncommon to hear statement such as: “The weather
station in New York City reported a total of 300 HDD for the month of
March”
Heat
Index Temperature
The purpose of the Heat Index is to
estimate the
apparent temperature a person experiences when taking into account warm
temperatures plus humidity. Normally the human body cools itself by
evaporating sweat from the surface of the skin. The process of
evaporation removes heat from the skin. When the humidity increases,
the ability to evaporate sweat from the skin surface is decreased,
which in turn decreases the ability to shed heat from the body. For
example when the air temperature is 85F with a low relative humidity of
40%, the apparent temperature to the body is the same as the regular
air temperature (85F), however, keeping the air temperature at 85F and
increasing the relative humidity to 70% results in making the human
body feel like it is actually 93F.
Max
‘Max’ is short for
‘Maximum’ and is most often used to describe the
highest value that a weather parameter reaches during a 24 hour day.
Usage of ‘Max’ with other time periods is typically
preceded by a reference to the time period, for example Monthly Max
Temperature would mean the highest temperature that occurred during a
month.
See also, the entry on wind for a comparison between wind speed and max wind speed.
Mean
In most cases,
‘Mean’ refers to
the arithmetic mean of a weather parameter. Specifically the sum of all
parameter members divided by the number of members. For example the
Daily Mean Wind Speed is the sum of the 24 hourly wind speed
observations divided by 24. The exception to this is often applied to
temperature where the Daily Mean Temperature has an established
convention of being the mean of the max and min temperature as opposed
to all available temperature observations. The reason for this
is that in the US there are nearly 10,000 cooperative weather
stations
that only record the daily max and min temperature (and total daily
precipitation and snowfall). In order for daily mean temperature to be
consistent across all stations, all stations must produce the
mean
using the same method. Thus even though a station may record 24 hourly
temperatures throughout the day, the Daily Mean Temperature is still
computed as the mean of the max and min temperatures so as to be
consistent with stations that ONLY record max and min
temperatures.
Note that any ‘special’ observations are not
typically used to produce the mean.
Min
‘Min’ is short for
‘Minimum’ and is most often used to describe the
lowest value that a weather parameter reach during a 24 hour day. Usage
of ‘Min’ with other time periods is typically
preceded by a reference to the time period, for example Monthly Min
Temperature would mean the lowest temperature that occurred during a
month.
Precipitation
Precipitation is any water based
particle falling
from the sky that reaches the ground including drizzle, freezing
drizzle, rain, freezing rain, snow, snow grains, snow pellets
(graupel),
sleet, hail, ice pellets and ice crystals. Weather Source provides
Precipitation as “inches of liquid water”. For
non-frozen precipitation (rain and drizzle), this is simply the direct
measurement of the precipitation. For frozen precipitation the
precipitation is melted and the depth is measured and recorded. For the
most part, with the exception of hail, one can safely assume that
precipitation that occurs when the temperature (at 2 meters above the
ground) is 34F or above will be rain. It is possible for snow to occur
and accumulate when the 2 meter temperatures are slightly above
freezing (32F) when the air aloft is cold enough to support snow. Also,
one can safely assume that precipitation that occurs when the 2 meter
temperature is below 30F will be of a frozen variety. For 2 meter
temperatures in between 30 and 34 degrees Fahrenheit, one often has to
reference other weather information, to determine what type of
precipitation occurred.
Instead of an amount of precipitation, you may see a report of "T" or "TRACE". Trace means that precipitation was observed falling, either by a human observer or an automated instrument, but the amount that fell was below the threshold of what the is measurable. For example a couple drops of rain, or a few stray flakes of snow. The amount is generally not evenenough to cover the surface. Generally less than 0.01 inch."
Relative
Humidity
Relative Humidity is a measure of how
much water
vapor is mixed into the air. The specific amount of water vapor that
can be mixed into the air is related to the temperature of the air.
Warm air can ‘hold’ more water vapor than cold air.
No matter what the air temperature is, there is a maximum amount of
water vapor air at that that air can hold. For that reason Relative
Humidity is provided as a percentage between 0% to 100%, where 0% means
the air contains no water vapor (a very rare occurrence) and 100% means
the air contains the maximum amount of water vapor for air at a
specific temperature. It is possible to have a Relative Humidity of
100% at nearly any temperature that can be found on Earth, however if
you were to “wring-out” the water from warm air you
would collect much more water than from cold air
Sea Level Pressure
Sea Level Pressure is the Atmospheric
Pressure
measure at a weather station that is mathematically adjusted to present
the pressure the station would measure if the station where at an
elevation equal to Sea Level (elevation of 0). Weather Source provides
Sea Level Pressure in units of millibars (mb).
Significant Weather
Significant weather observations are
reports of any
notable weather including any type of precipitation, fog, high winds or
other weather phenomenon that warrants notice to aviation and/or the
public.
Snowfall
Snowfall is the occurrence of
accumulating snow.
Weather Source provides observation of Snowfall in units of inches.
Station
Pressure
Station Pressure is the Atmospheric
Pressure
measure at a weather station. Weather Source provides Station Pressure
in units of millibars (mb).
Temperature
Unless otherwise noted, Weather Source
uses the
term ‘Temperature’ to refer to the temperature at a
height of 2 meters above the ground. This is the standard height at
which temperature at weather stations is observed. Weather Source
provides Temperature in units of degrees Fahrenheit.
Visibility
Visibility is provided in units of
miles. Prior to
using automated equipment to measure visibility, visibility was often
expressed without limit. For example some stations on a very clear day
may have recorded a visibility of 30 miles. With the adoption of
automated equipment, visibility is generally recorded to a maximum of
10 miles. Weather phenomenon such as fog, precipitation and haze can
significantly reduce visibility.
Wet
Bulb Temperature
Wet bulb temperature is the
temperature measure by
a wet bulb thermometer OR is derived mathematically as a function of
temperature, dew point temperature and station pressure. Wet bulb
temperature is the temperature air would have if the energy of the air
(air temperature) were used to evaporate water into the air until the
air became saturated (a relative humidity of 100%) assuming the air
pressure remained constant. Wet Bulb Temperature is similar to Dew
Point Temperature, except the process of achieving Wet Bulb Temperature
assumes that there is no limit on the supply of moisture.
Wind
and Maximum Wind Speed
Wind is the movement of air and is
expressed in
terms of direction and speed. The wind direction is the direction from
which the wind is blowing. For example, a “North
Wind” blows from the North to the South. Weather Source
provides Wind Direction in units of compass degrees with 90
representing East, 180 representing South, 270 representing West and
360 representing North. Zero (0) degrees is generally use to represent
calm conditions (no air movement). Wind Speed is provided in miles per hour.
Maximum Wind Speed
Maximum
wind speed (ie, max wind) is the highest wind speed reported each hour.
Max wind speed for any hour is calculated by taking the the greatest of
three values reported for each hour: (1) wind speed, (2) wind gust, and
(3) peak wind speed. Wind gusts and peak wind speed are not always
reported, in which case max wind would simply be the value of the
reported wind speed, and, hourly wind speed and the maximum wind speed
would be the same. It is not unusual for the max wind and the hourly
wind speed to be the same, as big wind events are infrequent. Wind
gusts and peak wind speed are only reported when certain criteria are
met. Gusts are only reported when the wind is characterized by rapid
fluctuations in wind speed with a variation of 10 knots (11.5 mph) or
more between peaks and lulls. In which case the maximum instantaneous
speed is reported as a gust. The peak wind is only reported whenever
the maximum instantaneous speed is greater than 25 knots (28.75 mph).
Wind
Chill Temperature
Wind Chill Temperature is a
temperature index
similar to Heat Index, but designed to represent how cold a person
feels when exposed to cold temperatures and windy conditions. Weather
Source provides Wind Chill in units of degrees Fahrenheit.
Here are some additional questions and answers.
Also, if there is a meteorological definition you have not found here, we suggest that you take a look at the American Meteorological Society Glossary of Meteorology and the United States National Weather Service Glossary.