Even though Automated Surface Observing System (ASOS) observations look similar to those produced by human observers, ASOS uses automated sensors and logical processes that differ from the human senses. It is important for ASOS users to know how ASOS arrives at its observation values. This and other ASOS algorithm lessons will assist you in understanding these processes.
Upon completion of this lesson you will be able to:
Use these links to move to various sections of this module.
This tutorial is structured so that you can progress through the primary tutorial material to achieve a basic understanding of how the ASOS pressure algorithm works. At various points throughout the tutorial, review questions are placed to test your understanding of the material. In addition, links are embedded within the tutorial text to provide additional information on specific topics.
This is a tutorial on the pressure algorithms used by the Automated Surface Observing System (ASOS). The purpose of this tutorial is to help you better understand what ASOS does in determining pressure and related parameters.
There are three reasons why you need to understand how ASOS obtains atmospheric data and processes this information into reportable values. First, a knowledge of the ASOS algorithms will allow you to better judge data quality and to more effectively conduct on-station quality control of ASOS observations. When ASOS is operating properly, it reports what it senses. Sometimes, however, you might ask: What is it sensing? An understanding of how ASOS works will help answer this infrequent question.
The second reason why you need to know how ASOS processes information deals with the system response to rapidly changing conditions. Because ASOS algorithms typically use a time average rather than a spacial average ( per the human process), a lag can exist in the ASOS response to rapidly changing weather conditions. You need to know when to expect this type of response from ASOS.
Lastly, ASOS users must realize that ASOS sensors and algorithms have certain limitations built into them. Although ASOS senses basically the same thing as the human observer, there are differences. These differences affect what is transmitted in an ASOS observation. You, as an ASOS user, need to be aware of these events in the background.
Once every ten seconds the two digital barometers (Class I system) or three digital barometers (Class II system) provide pressure readings for the observing site. The barometers are very accurate quartz barometers which are regularly checked for tolerance. These are located in the Acquisition Control Unit (ACU) usually inside a building. These units are vented to the outside to ensure observation of ambient pressure.
If you have a Class I system with two barometers, the six readings taken every minute are sent to algorithms for processing and comparison. If you have a Class III system with three barometers, the same process occurs but here you have three readings to compare.
If one or more of the 6 pressure values obtained during a one-minute period are missing, the sensor is automatically logged as "inoperative". It can only be returned to "operational status" by a maintenance technician.
Once the sensor data has been determined, the further processing by the pressure algorithms takes place so as to provide additional pressure parameter information which is especially useful for those in the aviation community.
The sensor, the aneroid barometer, senses pressure data once every ten seconds. This sensor is found as a black box inside the cabinet of ACU in the forecast office. There are six pressure samples every minute. These six samples are then linearly averaged to come up with a 1-minute average pressure value. Then depending on whether you have 2 barometers or 3 barometers, these 1-minute averaged pressure values are compared to determine which of those values will be reported in the observation that is transmitted. Then additional pressure parameters are computed.
The following steps are completed by the processing associated with the ASOS pressure algorithms.
Step 1: Determine the observed pressure value.
The pressure algorithm uses the 6 ten-second pressure samples from the previous minute to calculate the 1-minute averaged pressure value. If less than 6 of those 10-second samples are available for a sensor, the output value will be reported as missing and the sensor logged as "inoperative".
Step 2: Compare the 1-minute pressure values and calculate the output.
The output for the pressure algorithm is calculated by comparing the 1-minute average values of the sensors.
In a Class I System, if both average pressure values of the two sensors agree within 0.04 inch of each other, the lower of the two values will be output in the next observation. If the two sensors do not agree within 0.04 inch of each other, then this value is marked as missing.
In a Class II System, if all three sensors agree within 0.04 inch of each other, the lowest of the three values will be output. If only two out of the three sensors agree within 0.04 inch of each other, again the lower value will be output and the third sensor is logged as "inoperative".
Step 3: Compute the Field Pressure value for output.
By definition, the field pressure is the atmospheric pressure computed for a specific field elevation.
Using the 1-minute averaged pressure value (P) and 5-minute average temperature in degrees Rankine, field pressure (Pa) is calculated using the following formula:
where HZa = Pressure Sensor Elevation minus Field Elevation
and TR = Average ambient temperature in degrees Rankine
Step 4: Compute the Station Pressure value for output.
By definition, the station pressure is the atmospheric pressure computed for a specific station and location.
Using the 1-minute averaged pressure value, the system calculates station pressure first by computing the difference between sensor elevation (HZ) and station elevation (HP) using the equation:
The system then obtains the current average 5-minute temperature in degrees Rankine (TR) and the current pressure (P) and calculates station pressure using the following formula:
If TR is marked missing and the absolute value of HZP is less than or equal to 100 feet, station pressure is calculated using the following equation:
where: "AS" is the altimeter setting
Step 5: Compute the Sea Level Pressure value for output.
By definition, sea level pressure is the pressure value obtained by the theoretical reduction or increase of station pressure to sea level.
The system calculates sea level pressure by using 12-hour average ambient temperature to access the proper pressure reduction ratio value, then calculates sea level pressure using the following equation:
where Ps = Station Pressure
and R = Pressure Reduction Ratio
and C = Pressure Reduction Constant
Step 6: Compute the Pressure Altitude value for output.
By definition, pressure altitude is the altitude in the standard atmosphere at which a given pressure will be observed.
The system calculates pressure altitude (PA) using field pressure (Pa) and the following equation:
Step 7: Compute the Density Altitude value for output.
By definition, density altitude is the altitude in the standard atmosphere where air density is the equivalent to that at the airport.
The system calculates density altitude using the current 5-minute average temperature in degrees Rankine and current field pressure using the following equation:
Step 8: Compute the Altimeter value for output.
By definition, the altimeter setting is the pressure value to which an aircraft altimeter scale is set, so it will indicate the altitude above mean sea level of the aircraft on the ground at the location for which the pressure value was determined.
It is calculated using the field pressure (Pa) and field elevation of the pressure sensor (Ha) using the following equation:
If the field pressure is missing, average pressure (P) and elevation of the pressure sensor ( Hz) are used.
Step 9: Compute the Pressure Remarks.
The algorithms checks the remark criteria once each minute. Remarks are included in all observations, including the next hourly. Only the most current remark is included in the observation.
Remarks generated include PRESRR (Pressure Rising Rapidly), PRESFR( Pressure Falling Rapidly), and 3-hourly pressure change.
For rapid changes in pressure, the algorithm compares the current station pressure (Ps) with station pressure calculated 20 minutes (Ps 20) ago. The criteria the algorithm uses to create the rapidly rising and rapidly falling remarks are as follows:
The pressure change remark is retained through the next hourly.
The pressure tendency remark is also created for 3-hourly synoptic reports. Here, the algorithm compares the current station pressure to the station pressure recorded hourly for past three hours. If any of the pressures are missing, the remark created is 5////. The format for this element is 5appp where:
Once every minute, the current 1-minute average from the algorithm is used to obtain the reportable sea level pressure values and altimeter setting for use in the coded METAR observation.
The examples given below show a series of Class I and Class II sites with the ten-second pressure samples used in determining the 1-minute pressure values available for output to the coded METAR observations.
Computing the 1-minute pressure using the 6 consecutive ten-second samples to produce the next 1-minute average pressure output using a Class I site.
Site: Farmville, IA
|Time||Barometer A||Barometer B|
Comparing barometer A to barometer B:
A - B = 30.154 - 30.153 = 0.001
Since their difference is 0.001 which is less than 0.04 inch, both values are good. So the lowest of the two is taken as output pressure value for the next observation: 30.153 which is output as 30.15.
Computing the 1-minute pressure using the 6 consecutive ten-second samples to produce the next 1-minute average pressure output using a Class II site.
Site: Ranch City, SD
|Time||Barometer A||Barometer B||Barometer C|
Comparing barometers A, B, and C:
A - B = 30.152 - 30.154 = -0.002
B - C = 30.154 - 30.154 = 0.000
A - C = 30.152 - 30.154 = -0.002
Since these differences are less than 0.040 inch, then all 3 samples are useable. So we take the lowest of the three samples to use as output which will be 30.152 output as 30.15.
Computing the pressure from a Class II site with two barometers not in agreement with one another
Site: River City, ND
|Time||Barometer A||Barometer B||Barometer C|
Comparing these barometers:
A - B = 30.095 - 30.127 = 0.032
B - C = 30.127 - 30.168 = 0.041
A - C = 30.095 - 30.168 = 0.073
Since the differences between B - C and A - C were greater than 0.040 then the value for barometer C is not used. So the lowest pressure value from Barometers A and C is used, which is 30.095, which will be output as 30.10. Barometer C will be logged as "inoperative".
This tutorial discussed the various aspects of the ASOS pressure algorithms that provide the ASOS METAR observation with a value for sea level pressure and altimeter setting for related pressure parameters. It began with several reasons why you should know how ASOS algorithms work. It then briefly discussed the sensor and how, once every minute, the pressure algorithm computes a pressure reading by doing a linear average of the previous six 10-second samples. Also, it briefly discussed the pressure sensor and how it physically works. The steps used in the algorithm processing were then reviewed which included computing the following pressure parameters: (a) 1-minute pressure value; (b) field pressure; (c) station pressure;(d) sea level pressure; (e) pressure altitude; (f) density altitude; (g) altimeter setting; (h) pressure sensor remarks. The lesson concluded with three examples of ASOS pressure calculations. These provided a good review of how ASOS determines pressure values.
Chu, Roland, 1994: Algorithms for the Automated Surface Observing System (ASOS). ISL Office Note 94-4, NWS/OSD, 106pp.
Clark, P., 1994: "ASOS Trainer's Toolbox" series, various topics. Surface Observation Modernization Office, NWS.
Last updated 11/07/97