AIAA 2011-6385 AIAA Guidance, Navigation, and Control Conference 08 - 11 August 2011, Portland, Oregon Comparison of the Impacts of Airport Terminal/Surface Weather Hazards Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Shubh Krishna * , Rafal Kicinger, Ph.D. † , Girishkumar Sabhnani, Ph.D., ‡ and Jimmy Krozel, Ph.D. § Metron Aviation, Inc., Dulles, VA, 20166 This study analyzes the Air Traffic Management (ATM) impacts of surface/terminal weather constraints at the 35 busiest airports in the National Airspace System (NAS). The degradation in airport departure and arrival rate performance is investigated during time periods where ceiling, visibility, surface winds, freezing precipitation, and thunderstorms prevent clear weather throughput. Using cumulative distribution functions (CDFs), we compare airport performance during time periods when weather hazards are present with clear weather baseline performance. Comparing against the clear weather baseline as well as across weather hazard types allows us to rank the effects of various weather hazards. Weighting such results by the frequency of occurrence of the weather event allows us to identify the most costly weather hazards in the NAS for terminal area operations. Such information allows us to focus future ATM investments on those technologies that can best mitigate the most significant weather hazards affecting the NAS. All comparisons are performed with 2009 operational ATM data. Abbreviations AAR Airport Arrival Rate ADR Airport Departure Rate ASPM Aviation System Performance Metrics ATM Air Traffic Management C&V Ceiling and Visibility CDF Cumulative Distribution Function FAA Federal Aviation Administration GDP Ground Delay Program kts knots ft m METAR NAS nmi OEP SM TFMS WITI I. Introduction feet meters Meteorological Aviation Report National Airspace System nautical mile Operational Evolution Plan Statute Mile Traffic Flow Management System Weather Induced Traffic Index W eather is a major limiting factor in the National Airspace System (NAS) today. The average weather-related delays in the NAS are twice the average non-weather delays [KH03, KC03]. The Aviation Capacity Enhancement Plan [FAA03] lists weather as the leading cause (65% to 75%) of delays greater than 15 minutes, with terminal volume as the second leading cause (12% to 22% of delays). In prior work, we have investigated how to categorize a wide variety of aviation weather impacts [KM07, KMP08]. A review of the scientific analysis approaches that formulate Air Traffic Management (ATM) impact models is given by Krozel [K10], including surface/terminal, en route, as well as oceanic models. In this paper, we only focus only on surface/terminal impacts. In order to study airport capacity impacts, we compare surface/terminal area ATM impacts for a variety of weather phenomena. In the terminal/surface domain, weather constraints are caused by a large spectrum of weather phenomena: fog, haze, smoke, ceiling and visibility (C&V), thunderstorms, lightning, hail, heavy rain, in-flight icing (typically a terminal area constraint [KK08]), wind shifts, gusts, microbursts, wind shear, tornados, waterspouts, snow, blizzards, surface icing, and volcanic ash. However, not very many of these weather phenomena occurring at or near airports have been studied to determine the causality or ATM-impact (as surveyed in [K10]), and in many * Analyst, Research and Engineering Department, 45300 Catalina Ct, Suite 101 Sr. Analyst, Research and Engineering Department, 45300 Catalina Ct, Suite 101, AIAA Member ‡ Sr. Analyst, Research and Engineering Department, 45300 Catalina Ct, Suite 101, AIAA Member § Sr. Engineer, Research and Engineering Department, 45300 Catalina Ct, Suite 101, AIAA Associate Fellow 1 American Institute of Aeronautics and Astronautics † Copyright © 2011 by the American Institute of Aeronautics and Astronautics, Inc. All rights reserved. cases, there simply are insufficient data available to do the analysis. While related literature [Bu78, FAR08, Le07, Pa94, Tu95] provides information on pilot guidelines for addressing such aviation weather hazards in the NAS, most of the scientific analyses based on operational data for ATM impacts (see [K10]) focuses on en route convective weather hazards since they have such a large impact on the NAS over many days in the year. This paper aims at studying the surface/terminal area to better understand and compare the different weather hazards and to quantify how they impact the terminal/surface domain in terms of ATM performance. This paper is organized as follows. After this brief introduction, we provide background material on the process of analyzing ATM impacts. Then we present supporting analyses for a number of weather phenomena according to this process, including a section comparing all weather phenomena studied. Finally, we state our conclusions, and provide references. An appendix included at the end of the paper discusses results of a complementary analysis of weather impacts at major airports incurred during Ground Delay Programs (GDPs). Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 II. Background Next, we provide background material related to this effort. We describe the evaluation process and the data sources used for the impact analysis. A. Evaluation Process The process used to evaluate weather impacts on NAS resources is as follows. 1. Describe the type of weather whose impact is evaluated. In this paper, we focus on a subset of those weather phenomena identified in the Introduction. In particular, we address how ceiling, visibility, surface winds, freezing precipitation, and thunderstorms reduce clear weather throughput. 2. Determine the frequency of occurrence of weather states that cause an impact, expressed either as a number or, if available, the total annualized duration of events in the NAS. This may range from enumerating episodic cases for events that occur infrequently (e.g., volcanic ash on runways), or a full climatology for weather events that occur frequently throughout the year (e.g., convection or C&V). 3. Analyze the impacts on NAS performance for each weather phenomenon. The first aspect of this is to determine the clear weather baseline for the NAS resource, in this case, for each of the 35 busiest airports in the US, formerly known as Operational Evolution Plan (OEP) airports (Figure 1). Currently, 30 out of OEP-35 airports are included in the set of “core” airports. 4. Given the clear weather baseline and the frequency of occurrence, quantify the total ATM impact considering a weighted impact, weighting the ATM impact with the frequency of occurrence. The impact considered in this paper is the departure and arrival throughput degradation. These throughput reductions can be attributed to delays, GDPs (discussed in the Appendix), cancellations and diversions. Other types of surface delays, such as gate delay and taxi delay, are discussed where applicable. Cancellations and diversions are not discussed but may be analyzed as part of future work. B. Sources of Data The sources of traffic and weather data in this study include the following. • ASPM. The FAA currently provides Aviation System Performance Metrics (ASPM) data for flight metrics at 77 major airports, referred to as the ASPM airports. This set of 77 airports includes all OEP-35 airports. ASPM includes airport weather, runway configuration, and arrival and departure rates. Weather observations recorded for each of the ASPM airports come from Meteorological Aviation Reports (METARs). Figure 1. OEP-35 airports used in analysis (HNL airport not shown). 2 American Institute of Aeronautics and Astronautics • METARs. METARs are aviation routine weather reports that are typically issued once per hour at airports and permanent weather observation stations throughout the world. This standardized format is approved by the International Civil Aviation Organization (ICAO) to be readily understood worldwide. The primary users of METAR information are the aviation community. Hourly observations of temperature, dew point, wind speed and direction, precipitation, cloud cover and heights, visibility, and barometric pressure are typically reported in METARs. Standardized codes contained in a METAR message are summarized in Table 1 [FMH95]. • TFMS. The FAA’s Traffic Flow Management System (TFMS) provides detailed traffic demand information, including scheduled and filed flight plans, along with actual flight tracks. Table 1. METAR Code Descriptions. Qualifier Weather Type Intensity or Proximity Descriptor Precipitation Obscuration Other Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 - Light a Moderate + Heavy VC In the Vicinityb MI PR BC DR BL SH TS FZ Shallow Partial Patches Low Drifting Blowing Shower(s) Thunderstorm Freezing DZ RA SN SG IC PE GR GS Drizzle BR Mist PO Well Developed Rain FG Fog Dust/Sand Snow FU Smoke Whirls Snow Grains VA Volcanic Ash SQ Squalls Ice Crystals DU Widespread FC Funnel Dust Ice Pellets Cloud(s) SA Sand Hail (Tornado, or HZ Haze Small Hail/ Snow b Waterspout) Pellets PY Spray SS Sandstorm UP Unknown DS Duststorm Precipitation Note: The weather groups are constructed by considering columns 1 to 5 in sequence, i.e., intensity, followed by description, followed by weather phenomena a To denote moderate intensity no entry or symbol is used. b Tornados and waterspouts are coded +FC C. Clear Weather Baseline Throughput is highly variable due to a multitude of factors, including weather, congestion, and demand, so establishing a cause-and-effect relationship, and quantifying such a relationship, is challenging. Furthermore, analyzing capacity reductions due to weather impacts, we must compare weather impacted performance with performance that occurs during peak capacity conditions. Since weather is a large cause of degraded performance of the NAS, we consider clear weather as the most important peak capacity condition. We defined clear weather as the following: visibility of 10 miles; ceiling above the minimum visual approach; wind less than 10 knots; and no precipitation. The average departure and arrival throughput counts, stratified by airport, hour, weekday/weekend and season (summer, winter, and other (spring and fall combined)), is calculated for the entire year of 2009, for all hours with clear weather conditions. Thus, with 35 airports, 24 hours a day, and 6 sets of profiles (e.g., summerweekday) for each airport, a lookup table was created that represents the average of clear weather departure and arrival throughput counts per airport, per summer-weekday-hour, etc. The departure and arrival throughput observed during a weather impacted day/hour/airport is then compared with the clear weather baseline for that airport, accounting for weekday/weekend, season and hour; the difference in throughput represents the throughput degradation. D. Use of CDF Plots A CDF plot displays the proportion of X values less than or equal to x. In particular, X=x and Y=0.4 will mean that for 40% cases, X ≤ x. Consider the example of arrival throughput CDF plot shown in Figure 2. The x-axis represents arrival throughput rate (ratio of actual arrival count to the average arrival count, multiplied by hundred); the yaxis shows the percentile. The median, extended from the y-axis with the dashed horizontal line, intersects with the orange Figure 2. Example CDF Plot. 3 American Institute of Aeronautics and Astronautics and black CDF curves at x-axis values of 60% and 100%, respectively. In this example, the black CDF curve is the clear weather baseline; the distribution is symmetric and similar to a Gaussian and, expectedly, the median rate is 100%. The median of the weather impacted throughput rate distribution, shown in orange, is 60%. This means that half of all hours with the associated weather condition had arrival throughput that was 60% or less of the typical arrival throughput at the same airport and the same season, weekend/weekday, and hour. Multiple curves in the same throughput CDF plot can be compared in this way. For same value of X=x, a higher value of Y means more cases had less than of equal to x throughput percent. Similarly, for same value of Y=y, a smaller value of X conveys that same proportion of cases had lesser throughput percent. Thus a curve C1 that lies to the left and above curve C2 represents reduced throughput. Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 III. Impact Analysis The impact analysis focuses on frequency of occurrence and airport arrival throughput. We distinguish airport departure and arrival throughput from airport departure rate (ADR) and airport arrival rate (AAR); the latter being operational terms that represents the number of aircraft an airport can accept, whereas the former represents the actual throughput (departure or arrival) defined as the number of flights per hour at an airport. A. Ceilings Description. A ceiling is defined as “the height above the earth’s surface of the lowest layer of clouds or obscuring phenomena that is reported as “broken,” “overcast,” or “obscuration,” and not classified as “thin” or “partial” [AIM10]. A broken layer, the least restrictive of the ceiling definitions, is defined as a layer of the atmosphere with 5/8 to 7/8 sky cover. Full sky coverage is defined as “overcast.” Frequency of Occurrence. Actual hourly weather observations at OEP-35 airports were analyzed for year 2009 METAR data. Figure 3 shows the count of hourly observations with low ceiling, defined as 3000 feet (ft) or less. To ensure we are addressing time periods of significant ATM activity, only those hours where NAS-wide demand is typically the highest was compared with the clear weather baseline. Analysis of the aggregate departure and arrival counts across all airports showed that the hours of 0700 to 2000 local times are the busiest hours across the whole NAS - only observations occurring within this time period were used for the analyses of throughput in this paper. We group ceiling data into three tiers: 2000-3000 ft, 1000-2000 ft, less than 1000 ft; the breakdown of occurrence, by ceiling tier and airport, is shown in Figure 3. Since low ceilings are sometimes associated with SEA, SAN, ATL and LAX observe most hours with low ceilings, although for SAN ceilings below 1000 ft are relatively infrequent. Figure 3. Frequency of Low Ceiling for OEP-35 airports. 4 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 precipitation, the impact on throughput rate during low ceiling with and without precipitation are both analyzed. Impacts. We quantify the degradation in throughput observed during hours with low ceiling by comparing observed throughput during hours with low ceiling and comparing it against the clear weather baseline. The hours that are analyzed are restricted to 0700 and 2000 local time, in order to calculate degradation in performance when the system – in this case, the NAS – is busiest. The data is Percent of Average Clear Weather Arrival Throughput segregated in terms of weekend/weekday and Figure 4. Impact of low ceilings on arrival throughput. summer/winter/other, as the average demand is different in these periods. The throughput rate during the presence of low ceiling, as a percentage of the clear-weather baseline for similar hours at affected airports, is shown in Figure 4. The CDF of the arrival throughput during clear weather is compared to the CDF of throughput in the presence of low ceiling. Data for low ceilings is split into three ranges: between 2000 ft and 3000 ft, between 1000 ft and 2000 ft and less than 1000 ft. For both departure and arrival throughput, there is approximately 3-5% reduction in throughput in presence of low ceilings. This is measured by comparing the integral (or cumulative sum) of the low ceiling CDF curve and the integral of the baseline CDF curve. Since the low ceiling curve is to the left of the baseline, there is associated throughput degradation. The relatively small throughput reduction during low ceiling time periods is because a majority of OEP-35 airports have flexibility to mitigate those weather conditions without impacting scheduled demand. However, airports with scheduled demand approaching operational limits are much more sensitive, and more disproportionately affected, to weather conditions of all types. As such, the regional impact of low ceiling can vary greatly, even if the aggregated statistics across all OEP-35 airports only show a small impact. GDPs are used to mitigate these circumstances at congested airports; a complementary analysis of GDPs is discussed further in the Appendix B. Visibility Description. Visibility is the ability, as determined by atmospheric conditions and expressed in units of distance, to see and identify prominent unlighted objects by day and prominently lighted objects by night. Visibility is reported as statute miles (SM), hundreds of feet (ft) or meters (m) [AIM10]. Frequency of Occurrence. Actual hourly weather observations were analyzed to determine hourly counts when low visibility (below 3 SM) was observed as shown in Figure 5. We separate the hours when only low visibility was observed from hours when low visibility occurred in presence of other weather factors (i.e. precipitation) that could affect the airport throughput. Figure 5 shows that low visibility co-exists with some other weather event, such as rain or snow. Because low visibility can be thought of as a secondary effect, or consequence, of a weather event, it is difficult to analyze in isolation. Thus, virtually all causes of low visibility are already analyzed in this paper with the analyses of the multitude of other weather types (rain, snow, fog, drizzle, etc.) Impacts As previously mentioned, low visibility co-exists as a secondary effect of a variety of weather conditions. Most of these weather conditions are already analyzed separately in this paper: rain, snow, drizzle, fog, thunderstorms. The impacts of these conditions are compared in Section IV. C. Surface Winds Description. Surface winds are winds reported by METAR observations. Surface winds are conventionally measured at a height of 10 m above ground in an area where the distance between the anemometer and any obstruction is at least 10 times the height of the obstruction. In reference to a particular runway, surface winds can act as headwinds, tailwinds, or crosswinds. High surface winds are typically accompanied by gusts in which the wind speed increases suddenly. Frequency of Occurrence. Hourly counts of actual weather observations when strong winds (speed > 20 kts) were observed are shown in Figure 6. We separate the hours when only strong winds were present and when strong winds existed in presence of other factors that could affect the airport throughput. Other factors included low C&V, moderate or heavy rain, snow, fog, thunderstorms, and other conditions in the vicinity of the airport. 5 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Figure 5. Frequency of Low Visibility for OEP-35 airports. The data shows most hours with strong surface winds at OEP-35 airports do not have another co-existing weather condition. This is in stark contrast to what was shown for visibility. Thus, winds are a good candidate for an independent evaluation for ATM impact, as it is easily isolated from other impacting weather conditions. Figure 6. Frequency of Strong Winds for OEP-35 airports. Crosswind and tailwind components were analyzed separately. For each airport, we analyzed the wind direction, wind speed, and the runway configuration in use at that hour to compute the tailwind and crosswind components. Figure 7 shows the frequency density plot of tailwind (headwind) vs crosswinds. As expected, airports mostly operate with tailwinds < 8 kts; however, crosswinds go as high as 20 kts. 6 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Impacts. We quantify the degradation of throughput during periods of strong winds. Clear weather baseline consisted of average arrival throughput counts observed during times when wind speed < 10 kts. The data is segregated in terms of weekend/weekday and summer/winter/other as described earlier. We consider the crosswind impact separately from the tailwind impact. The baseline data represents clear weather averages and is same as that is used in analyses of all other weather types in this paper. Dark black density represents data point with number of hours > 5000, with numbers linearly decreasing with the shade of grey. Tailwinds (kts) Headwinds (kts) Figure 7. Headwinds vs Crosswinds frequency density plot for OEP-35 airports for 2009. Figure 8 shows the arrival throughput rate during the presence of strong winds, as a percentage of the clear-weather baseline for similar hours at affected airports. It shows that arrival throughput is reduced by 3-5% in presence of high tailwinds/crosswinds. Crosswinds > 15 kts seem to have more impact on throughput as compared to tailwinds > 5 kts; however, it must be noted that airports often change their runway configurations shortly after suboptimal Percent of Average Clear Weather Arrival Throughput wind conditions, such as tailwinds, Figure 8. Arrival throughput in presence of strong winds. develop; thus there is a much lower sample size to analyze for tailwinds. Figure 9 shows the number of hours, after a sudden change in wind speed and/or direction is detected, until a runway configuration change (RCC) takes place. A majority of the RCCs takes place within four hours of the wind profile change, including more than 25% that occur within one hour. D. Freezing Precipitation Description. Freezing precipitation (i.e. snow, ice pellets, freezing rain, or a combination thereof) can cause icing on the surfaces of aircraft and runways, posing a safety hazard for aircraft. It is a common occurrence from December through March in the middle latitudes of the Continental US (CONUS). Frequency of Occurrence. Hourly METAR observations at OEP-35 airports were analyzed for 2009. Hours where one of the following weather conditions present were identified: Light Snow Freezing Drizzle Moderate Snow Freezing Rain Heavy Snow 7 American Institute of Aeronautics and Astronautics RCC Counts Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Hours Following Wind Event Figure 9. Number of Hours between Wind Event ** and Runway Configuration Change. The counts of hourly observations having each of these weather types are shown in Figure 10. Light snow is the predominant frozen precipitation that was observed. Impact Analysis. We quantify the degradation in throughput, defined as the number of flight departures and arrivals per hour at an airport, observed during periods of freezing precipitation at the surface. Snow observations were categorized based on precipitation intensity. METAR categorizes precipitation intensity into three levels: light (-), moderate ( ), and heavy (+). For example, -SN, SN and +SN represent light snow, moderate snow and heavy snow, respectively. Freezing rain and freezing drizzle are denoted in the METARs as FZRA and FZDZ, respectively. Figure 10. Number of Hourly Observations for Frozen Precipitation Types. ** Wind Event is defined as a sudden change in direction and/or speed 8 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 The departure and arrival throughput rates during the presence of frozen precipitation, as a percentage of the clear-weather baseline for similar hours at affected airports, are shown in Figure 11. Throughput degradation shown in the CDFs can generally be assessed and quantified as follows: the further left the CDF of throughput rate for a particular weather type is from the clear weather baseline CDF, the greater the throughput degradation observed. For example, in Figure 11a, light snow corresponds to some departure throughput degradation, as it is to the left of the clear weather baseline CDF; however, moderate and heavy snow correspond to much higher throughput reductions. In fact, there was no departure throughput for 10% of hourly observations with moderate snow and more than 20% of hourly observations with heavy snow. This type of airport shutdown only occurred with light snow in 2% of the hourly observations. The ranking for impact of winter weather types on departure and arrival throughput, in descending order of highest magnitude of impact to lowest magnitude, is also displayed in Figure 11a and Figure 11b, respectively. Heavy Snow Moderate Snow Freezing Drizzle Freezing Rain Light Snow Baseline Heavy Snow Moderate Snow Freezing Drizzle Freezing Rain Light Snow Baseline (a) Departures (b) Arrivals Figure 11. Throughput Rate in the Presence of Frozen Precipitation. The reasons for the significant arrival throughput degradation in the presence of frozen precipitation include GDPs, along with strategic cancellations by the airlines in anticipation of the winter weather event. Cancellations of scheduled departures are also a significant component of the departure throughput reduction. Another significant reason is the gate and taxi-out delays that occur because of deicing. The precipitation type and the surface temperature determine the length of holdover time for deicing. If the precipitation rate, or liquid water equivalent, of the frozen precipitation is high, aircraft may have trouble meeting the holdover times that are required in order to takeoff. If holdover times are exceeded, aircraft must deice again, further increasing delays. Figure 12 shows a box plot for the distribution of gate delays and taxi out delays for each flight that departed during hours with frozen precipitation. The gate and taxi out delays for each flight were obtained from ASPM and 93,274 flights were analyzed. The horizontal line in the middle of the box represents the median gate or taxi-out delay; the lower and upper side of the box represents the 25th and 75th percentile, respectively. The length of the box represents the Interquartile Range (IQR). . The upper “fence” is 1.5*IQR above the 75th percentile; the lower fence is 1.5*IQR below the 25th percentile. Data outside of these ranges are outliers and are not shown. Figure 12 shows that there is an increase in gate and taxi out delays during frozen precipitation. In particular, there variance of the gate and taxi-out times markedly increase during hours of moderate or heavy snow, such that there are some flights absorbing an extraordinary amount of gate and taxi out delays. This large increase is likely due to deicing along with impaired movement at the airport due to weather conditions. E. Thunderstorms Thunderstorms. A thunderstorm is a local storm produced by a cumulonimbus cloud and accompanied by lightning and thunder, usually with strong gusts of wind, heavy rain, and hail that occur as a consequence of atmospheric instability. A strong convective updraft is present in the early stages of a thunderstorm, while a strong downdraft occurs in a column of precipitation during its dissipation. Frequency of Occurrence. Actual hourly weather observations were analyzed and the counts of hourly observations when a light (-TS), moderate (TS), severe (+TS) thunderstorm, or a thunderstorm in the vicinity of an airport 9 American Institute of Aeronautics and Astronautics (VCTS) was reported are shown in Figure 13. MCO and FLL experienced the longest duration of overall thunderstorm activity while FLL, MEM, and ATL were the airports most affected by severe thunderstorm activity. Heavy Snow Moderate Snow Light Snow Freezing Drizzle Freezing Rain Clear Weather Baseline Figure 12. Distribution of Gate and Taxi-Out Delays (for all flights departing during frozen precipitation). Thunderstorm in the Vicinity of an Airport (VCTS) Light Thunderstorms (-TS) Moderate Thunderstorms (TS) Heavy Thunderstorms (+TS) Total Hours Observed Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Gate Delay Taxi Delay Figure 13. Frequency of thunderstorms for OEP-35 airports 10 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Impacts. We quantify the degradation in throughput observed during hours of light, moderate, and severe thunderstorms, and (+TS) Heavy thunderstorms in the vicinity of an airport Thunderstorms against the clear weather baseline. This clear weather baseline is computed in the same way as described in our ceiling analysis. Figure 14 shows that arrival throughput is reduced by (-TS) Light about 8-15% in presence of thunderstorms. As Thunderstorms (VCTS) Thunderstorms expected, severe thunderstorms (+TS) cause in the Vicinity of an the largest throughput reduction as the Airport corresponding CDF curve is most shifted to the left. Figure 14 also indicates that light (TS) Moderate thunderstorms (-TS) appear to have more Thunderstorms adverse effect on airport throughput than moderate thunderstorms (TS). However, median throughput reductions for light and Clear Weather moderate thunderstorms are very similar (both Baseline curves cross the horizontal line at y=0.5 at very similar values of x). Finally, thunderstorm activity in the vicinity of airport (VCTS) has the least impact on throughput. Interestingly, in some case (see upper right Figure 14. Arrival Throughput in the Presence of part of Figure 14) thunderstorm activity in the Thunderstorm Activity. vicinity of the airport leads to arrival throughput increase as compared to the clear weather baseline. This may be explained by changes in operational procedures employed by air traffic controllers when a thunderstorm approaches the airport. Air traffic controllers typically attempt to streamline arrival procedures to accommodate the largest number of arriving flights and avoid airborne delays and diversions. This hypothesis is further confirmed by an analysis of the departure throughput (not shown) which does not show any throughput increases when thunderstorms appear in the vicinity of airports. On the contrary, in this case the departure throughput reduction is much more profound and very close to departure throughput reduction caused by moderate thunderstorms. Hence, when a thunderstorm approaches an airport, air traffic controllers tend to prioritize arriving flights thus increasing arrival throughput and decreasing departure throughput and with respect to clear-weather baseline. IV. Comparison In this section, we consider both the frequency of occurrence and the ATM impact, comparing all weather impacts to each other using CDFs as the basis of comparison. Figure 15 compares the CDFs for various weather types. The CDF of the clear weather baseline is also included for comparison purposes. The ranking of weather type, from highest to lowest impact, is displayed in the plot. Heavy snow has the highest impact on departure throughput degradation, while low ceiling (with no precipitation) having the least impact. Likewise, a comparison of arrival throughput with the clear weather baseline is shown in Figure 16. Frozen precipitation categories are in the top 4 list, in terms of impacting throughput, for both departures and arrivals. Figure 17 compares the magnitude of impact with frequency of occurrence, for each weather type studied in this paper. While moderate/heavy snow and freezing rain/drizzle has the highest impact on throughput degradation, it occurs much less frequently over the entire year compared with various other weather types. The magnitude of throughput degradation relative to the clear weather baseline is calculated by taking the integral (cumulative sum) of the CDF curve for each weather condition and dividing that by the integral of the CDF of the clear weather baseline. This provides an estimate of the average throughput degradation across all OEP-35 airports for each weather type. The frequency of occurrence is calculated by aggregating all hourly observations for each weather type across all OEP-35 airports during 2009. The magnitude of impact multiplied by the frequency of occurrence provides some measure of cost of surface weather hazards to the NAS system as a whole; however, there are many other variables involved in the systemic cost of surface weather hazards on the NAS, such as delay propagation, cancellations, fleet mix at impacted airports, etc. 11 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Figure 15. Comparison of Departure Throughput Rate with Clear Weather Baseline. Figure 16. Comparison of Arrival Throughput Rate with Clear Weather Baseline. 12 American Institute of Aeronautics and Astronautics Magnitude of Impact Frequency of Occurrence Heavy Snow Moderate Snow Freezing Drizzle Freezing Rain Heavy Thunderstorm Fog Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Low Ceiling with Rain Arrivals Departures Wind (30 kts or greater) Light Snow Drizzle Light/Moderate Thunderstorm Low Ceiling (No Precip) Average Percent Reduction in Throughput (relative to Clear Weather Baseline) Total OEP-35 Airport Hours Figure 17. Comparison of Magnitude of Impact with Frequency of Occurrence V. Conclusions This study analyzes the ATM impacts of surface/terminal weather constraints at the 35 largest (OEP-35) airports. The degradation in airport departure and arrival throughput is investigated during time periods where ceiling, visibility, surface winds, freezing precipitation, and thunderstorms are impacting the airport. Using CDFs, we compare time periods when weather hazards are present to time periods when there is a clear weather. Comparing against the clear weather baseline across multiple weather hazard types, we rank the effects of weather hazards. Heavy/moderate snow, freezing drizzle/rain, and heavy thunderstorms have the greatest magnitude of impact on both departure and arrival throughput at OEP-35 airports. However, weighing by frequency of occurrence, low ceiling has the most aggregated impact over the entire year. This is corroborated by an analysis showing that the most impacting condition for GDPs is low ceilings. Another interesting result from our analyses shows that during hours with light snow or thunderstorms approaching an airport, there is sometimes an increase in throughput relative to what typically occurs during clear weather. In the case of light snow, this may happen because the onset of light snow typically (in case of synoptic scale winter storms) precedes moderate or heavy snow and airlines may increase their operations before the worst of the weather arrives. Similarly, in the case of a thunderstorm approaching an airport, air traffic controllers may prioritize arriving flights thus increasing arrival throughput with respect to clearweather baseline to avoid airborne delays and diversions. The results of our analyses should be useful for developing predictive models of the impact of terminal weather on airport operations. We are planning to develop such models for major types of terminal weather hazards, including snow and freezing precipitation as such models are needed to improve traffic flow management planning. Acknowledgments This research was funded in part by NASA Ames Research Center, under contract NNA11AA17C, Weather Translation Models for Strategic Traffic Flow Management, and by FAA contract DTFAWA-10-D-00033, Weather Integration Technology. The authors appreciate the support of the NASA contract monitor, Mr. William Chan, and the FAA contract monitor, Mr. Dave Pace, in the course of this work. 13 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Appendix This Appendix contains an analysis of GDPs. It is common for the Air Traffic Control System Command Center (ATCSCC) to establish GDPs to address problems caused by reduced capacity at airports. GDPs work by metering the rate at which traffic can use a NAS resource. The scheduled demand for that resource may exceed its capacity over some time period, necessitating this Traffic Flow Management (TFM) action. In a GDP, the resource being rationed is an airport, for flights arriving at that airport. Using data from the FAA’s TFMS, we analyzed all the GDPs issued during 2009. Aggregate delay statistics categorized by various impacting conditions are shown in Table 2. The cause of each GDP, represented by the field “IC_CAUSE”, was counted for each OEP-35 airport. The distribution of GDPs, categorized by OEP-35 airport and impacting condition, is shown in Figure 18. Figure 19 shows the percentage of hours between 12 p.m. and 10 p.m. local time where the scheduled demand is at least 90% of the airport’s AAR limit. A strong relationship between frequency of GDPs and airports that often have scheduled arrival demand approaching their AAR limits can be seen amongst the airports highlighted in red font †† . This relationship also shows that weather has a more severe impact at airports with scheduled operations approaching operational limits. Type Thunderstorms Low Ceiling Low Visibility Wind Snow/Ice Table 2. Aggregate GDP Statistics for 2009 Total EDCT Controlled Flights Total EDCT Delay Minutes 101,579 10,105,167 281,137 23,268,239 40,089 3,197,686 184,777 14,297,538 57,580 6,835,458 Figure 18. Number of GDPs by Impacting Condition for OEP-35 airports. †† SFO is a special case, where GDPs are often implemented due to routine instances of low ceiling and fog 14 American Institute of Aeronautics and Astronautics Downloaded by UNIVERSITY OF ADELAIDE on October 27, 2017 | http://arc.aiaa.org | DOI: 10.2514/6.2011-6385 Figure 19. Comparison of Scheduled Arrival Demand relative to operational AAR. 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