Aviation Weather Services, Advisory Circular 00-45G Change 1 (July 2010) HQ JHH HI HJ ІНК HL N нỌ HP HQ HR JH IP IS
JL JMA KG кН JN ¡JO JP
KJ KK KL JR JS KN LG КР KQ KS LM LM MG MI MJ MK MIL MMILX MN LN MO ILO LP ¡LO OG OI NI lau NJ INK NL NM NN INO 1 INP NO MO INR MR NS PH OL OM ON 100 OP PJ OR ros G PL ГРМ PN 4 PO Ipp PQ PR PS PT RH RI OM ON 00 OP RJ RK AL rOs OT RN
SH SI SJ SK RO AR RS IRT
TH ITJ TK S SQ ISR SS ST TM
I TO I TP Figure 3-14. SD/ROB Digital Section Information Plotted on a PPI Grid Overlay Example (See Table 3-11 for Intensity Level Codes 1 through 6.)
3.3.2 Examples GRB 1135 AREA 4TRW+ 9/101 133/76 54W MT 310 45/47 C2428 AUTO Green Bay, Wisconsin, automated Radar Weather Report at 1135 UTC. An area of echoes, 4/10 coverage, contained thunderstorms and heavy rain showers. Area is defined by points (referenced from GRB radar site) at 9 degrees, 101 nautical miles and 133 degrees, 76 nautical miles. These points, plotted on a map and connected with a straight line, define the center line of the echo pattern. The width of the area was 54 nautical miles; i.e., 27 nautical miles either side of the center line. Maximum top was 31,000 feet MSL located at 45 degrees and 47 nautical miles from Green Bay. Cell movement was from 240 degrees at 28 knots.
ICT 1935 IN 9TRWX 274/84 216/93 22W MTS 440 260/48 C2131 AUTO Wichita, Kansas, automated Radar Weather Report at 1935 UTC. A line of echoes, 9/10 coverage, contained thunderstorm with intense rain showers. The center of the line extended Section 3: Observed Text Products Page 3-54
Aviation Weather Services, Advisory Circular 00-45G Change 1 (July 2010) from 274 degrees, 84 nautical miles to 216 degrees, 93 nautical miles. The line was 22 nautical miles wide.
To display graphically, plot the center points on a map and connect the points with a straight line;
then plot the width. Since the thunderstorm line was 22 nautical miles wide, it extended 11 nautical miles either side of your plotted line.
The maximum top is 44,000 feet MSL at 260 degrees, 48 nautical miles from Wichita. Cell movement was from 210 degrees at 31 knots.
GGW 1135 AREA 3S- 95/129 154/81 34W MT 100 130/49 0805 AUTO
Glasgow, Montana, automated Radar Weather Report at 1135 UTC. An area, 3/10 coverage, of light snow. The area’s centerline extended from points at 95 degrees, 129 nautical miles to 154 degrees, 81 nautical miles from Glasgow. The area was 34 nautical miles wide. The maximum top was 10,000 feet MSL, at 130 degrees, 49 nautical miles from Glasgow. Cell movement was from 80 degrees at 5 knots.
JGX 2235 AREA 2TRW++6R- 67/130 308/45 106W MT 380 66/54 C2038 AUTO
Atlanta, Georgia, automated Radar Weather Report at 2235 UTC. An area of echoes, total coverage 8/10, with 2/10 of thunderstorms with very heavy rain showers and 6/10 coverage of light rain (This suggests that the thunderstorms were embedded in an area of light rain). The area was 53 nautical miles either side of the line defined by the two points, 67 degrees, 130 nautical miles and 308 degrees, 45 nautical miles from Atlanta. Maximum top was at 38,000 feet and was located on the 66 degree radial of JGX at 54 nautical miles. Cell movement was from 200 degrees at 38 knots.
HKM 0235 CELL TRW+ 19/22 D5 MT 270 18/23 C0414 AUTO
Kohala, Hawaii, automated Radar Weather Report at 0235 UTC. A cell, containing thunderstorms with very heavy rain showers, 5 miles in diameter, was located 19 degrees, 22 nautical miles from Kohala. Maximum top was 27,000 feet located at 18 degrees, 23 nautical miles from Kohala. Movement was from 40 degrees at 14 knots.
TLX 0435 PPINE AUTO
Oklahoma City, Oklahoma, automated Radar Weather Report at 0435 UTC, detected no echoes.
Section 3: Observed Text Products Page 3-55
Aviation Weather Services, Advisory Circular 00-45G Change 1 (July 2010) KATE KCBW KMSX *KMBX
KRIX KOTX KGGW O KMYX KDLH OKTEX OKBIS УСУХ кРОІ KELX KABR O КИРУ KGRB C KSEX KRIW KUDX KFSD O KARY KCỂR 2 KOKX OKEHX KBBX aRx кИІХ KCYS KLAX KOAX O * KDMx KI wx KCLEO KOBZ ÖKDIX KDAX OKRGE *KUEX KILY O OKILN KRLX KLWX * KMUx KICK IGIX KPUX O KFTGO O KGLD KTWXO OKEAX KIND. KJL KFCIO OKAKQ
KDDCO OKSGF OKHES КУВХ О КЕУХО ~ÖKVTX KP≤x KABX EUN& KING KERX OKLTX O KINKY KIWA ОКАМА DEFDR CATLE KLZK ксихо квих КИГА OKCIX KYUX KHỐX OKLBB KMXX O KJCX KEMX CHEPZ KMAF OKFWS OKSHV КРОЕ KJAN KE OXO O KVAR OKIAX KCEK O RICH КМОВ LPLA OKMLE
DEX KEWE KHGX KIEWO O KAMX
PAECIO PAPD OKCEP A KBRO
PAHG SEC PHIMO T CER RKSGIO PAIH PHKM O
POTA ( RKIK Figure 3-15. WSR-88D Weather Radar Network Sites Section 3: Observed Text Products Page 3-56
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010) 4 RADA R AND SATELLITE IMAGERY
4.1 Radar
4.1.1 Description Radar images are graphical displays of precipitation and non-precipitation targets detected by weather radar. WSR-88D Doppler radar displays these targets on a variety of products which can be found on the internet on the National Weather Service (NWS) Doppler Radar Images web site at: http://radar.weather.gov/ridge/.
4.1.2 Modes of Operation The WSR-88D Doppler radar has two operational modes, Clear Air and Precipitation.
4.1.2.1 Clear Air Mode In Clear Air Mode, the radar is in its most sensitive operation. This mode has the slowest antenna rotation rate which permits the radar to sample the atmosphere longer. This slower sampling increases the radar's sensitivity and ability to detect smaller objects in the atmosphere. The term "clear air" does not imply "no-precipitation" mode. Even in Clear Air Mode, the WSR- 88D can detect light, stratiform precipitation (e.g., snow) due to the increased sensitivity.
Many of the radar returns in Clear Air Mode are airborne dust and particulate matter. The WSR- 88D images are updated every 10 minutes when operating in this mode.
4.1.2.2 Precipitation Mode Precipitation targets typically provide stronger return signals to the radar than nonprecipitation targets. Therefore, the WSR-88D is operated in Precipitation Mode when precipitation is present although some non-precipitation echoes can still be detected in this operating mode.
The faster rotation of the WSR-88D in Precipitation Mode allows images to update at a faster rate approximately every 4 to 6 minutes.
Section 4: Radar and Satellite Imagery Page 4-1
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010)
4.1.3 Echo Intensities
Figure 4-1. WSR-88D Weather Radar Echo Intensity Legend
The colors on radar images represent different echo reflectivities (intensities) measured in dBZ (decibels of Z). The dBZ values increase based on the strength of the return signal from targets in the atmosphere. Each reflectivity image includes a color scale that represents a correlation between reflectivity value and color on the radar image. Figure 4-1 depicts these correlations. The scale ranges from -30 to greater than 75 dBZ. The scale also include ND correlated to black which indicates no data was measured.
Reflectivity is correlated to intensity of precipitation. For example, in Precipitation Mode, when the dBZ value reaches 15, light precipitation is present. The higher the indicated reflectivity value, the higher the rainfall rate. The interpretation of reflectivity values is the same for both Clear Air and Precipitation Modes.
Reflectivity is also correlated with intensity terminology (phraseology) for air traffic control purposes. Table 4-1 defines this correlation.
Table 4-1. WSR-88D Weather Radar Precipitation Intensity Terminology Reflectivity (dBZ) Ranges Weather Radar Echo Intensity Terminology <30 dBZ Light 30-40 dBZ Moderate >40-50 dBZ Heavy 50+ dBZ Extreme
Section 4: Radar and Satellite Imagery Page 4-2
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010) Values below 15 dBZ are typically associated with clouds. However, they may also be caused by atmospheric particulate matter such as dust, insects, pollen, or other phenomena.
The scale cannot be used to determine the intensity of snowfall. However, snowfall rates generally increase with increasing reflectivity.
4.1.4 Products The NWS produces numerous radar products of interest to the aviation community. The next section will discuss Base Reflectivity and Composite Reflectivity both available through National Weather Service (NWS) Doppler Radar Images web site at:
http://radar.weather.gov/ridge/
4.1.4.1 Base Reflectivity Base Reflectivity is a display of both the location and intensity of reflectivity data. Base Reflectivity images encompass several different elevation angles (tilts) of the antenna. The Base Reflectivity image currently available on the ADDS website begins at the lowest tilt angle (0.5°), more specifically 0.5° above the horizon.
Both a short range (Figure 4-2) and long range (Figure 4-3) image is available from the 0.5º Base Reflectivity product. The maximum range of the short range Base Reflectivity product is 124 NM from the radar location. This view will not display echoes farther than 124 NM from the radar site, although precipitation may be occurring at these greater distances. Other options to view precipitation beyond 124 NM from the radar site include selecting the longrange view which increases coverage out to 248 NM, selecting adjacent radars, or viewing a radar mosaic.
Figure 4-2. WSR-88D Weather Radar Short Range (124 NM) Base Reflectivity Product Example Section 4: Radar and Satellite Imagery Page 4-3
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010) DBZ Radar Image from lational Weather Service: КРАН 19:03 UTC 04/29/2005 + Kankakee + Fort Wayne Lamoni • Peoria + Logansport • Limà + Kirksvill + Champaign.
• Quincy Spring field taindianapolis + Terre Haute + Bloomington Columbia Clinton + Louisville 50 Evansville, + Springfield ring Green
• Branson #79 1 yersbur + Crossville 25 + Lawrencebury 20 AMemphis + Chattangoga Little Rock Horence « Huntsvite 15 + Pine Blurg:" * + Oxford Tupelo + Rame 10 + Gadsden + Columbus + Binangham.
+ El Dorado & Greenville + Tuscaloosa J INDI Radar Image from National Weather Service: KPAH 19:03 UTC 04/29/2005 Figure 4-3. WSR-88D Weather Radar Long Range (248 NM) Base Reflectivity Product Example
4.1.4.1.1 Base Reflectivity Use The Base Reflectivity product can be used to determine the location of precipitation and nonprecipitation echoes, the intensity of liquid precipitation, and the general movement of precipitation when animating the image.
If the echo is precipitation, the product can be used to determine if it is convective or stratiform in nature. Stratiform precipitation (Figure 4-4) has the following characteristics:
Widespread in areal coverage, Weak reflectivity gradients, Precipitation intensities are generally light or moderate (39 dBZ or less),
• Occasionally, precipitation intensities can be stronger Echo patterns change slowly when animating the image.
Section 4: Radar and Satellite Imagery Page 4-4
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010)
Figure 4-4. WSR-88D Weather Radar Stratiform Precipitation on the 0.5º Base Reflectivity Product Example
Hazards associated with stratiform precipitation include possible widespread icing above the freezing level, low ceilings and reduced visibilities.
Convective precipitation (Figure 4-5) can be described using the following characteristics:
Figure 4-5. WSR-88D Weather Radar Convective Precipitation on the 0.5º Base Reflectivity Product Example
Section 4: Radar and Satellite Imagery Page 4-5
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010) Echoes tend to form as lines or cells, Reflectivity gradients are strong, Precipitation intensities generally vary from moderate to extreme,
• Occasionally precipitation intensities can be light Echo patterns change rapidly when animating the image
Numerous hazards are associated with convective precipitation. They include: turbulence, low- level wind shear, strong and gusty surface winds, icing above the freezing level, hail, lightning, tornadoes and localized IFR conditions with heavy precipitation.
4.1.4.1.2 Strengths of Base Reflectivity The strengths of the Base Reflectivity product include:
The location of precipitation and non-precipitation echoes is depicted, and The intensity and movement of precipitation is relatively easy and straight forward to determine.
4.1.4.1.3 Limitations of Base Reflectivity Limitations associated with the Base Reflectivity product include:
The radar beam may overshoot targets, and The image may be contaminated by:
o Beam blockage o Ground clutter o Anomalous Propagation (AP) and o Ghosts.
4.1.4.1.3.1 Radar Beam Overshooting Radar beam overshooting may occur because the radar beam (typically the 0.5 degree slice) can be higher than the top of precipitation. This will most likely occur with stratiform precipitation and low-topped convection. For example, at a distance of 124 NM from the radar, the 0.5º Base Reflectivity radar beam is at an altitude of approximately 18,000 feet; at 248 NM the beam height is approximately 54,000 feet. Any precipitation with tops below these altitudes and distances will not be displayed on the image. Therefore, it is quite possible that precipitation may be occurring where none appears on the radar image.
4.1.4.1.3.2 Beam Blockage Beam blockage (Figure 4-6) occurs when the radar beam is blocked by terrain and is particularly predominant in mountainous terrain. This impacts both the Composite Reflectivity and Base Reflectivity images.
Beam blockage is most easily seen on the 0.5º Base Reflectivity images where it appears as a pie-shaped area (or areas) perpetually void of echoes. When animating the imagery, the beam blockage area will remain clear of echoes even as precipitation and other targets pass through.
Section 4: Radar and Satellite Imagery Page 4-6
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010) shone Beam Blockage + A† + Burie y Soda Springs Malad City + Prestor + Logant
- Brigham City * Ogden Figure 4-6. WSR-88D Weather Radar Beam Blockage on Base Reflectivity Product Example
4.1.4.1.3.3 Ground Clutter Ground clutter (Figure 4-8) is radar echoes returns from trees, buildings, or other objects on the ground. It appears as a roughly circular region of high reflectivities at ranges close to the radar. Ground clutter appears stationary when animating images and can mask precipitation located near the radar. Most ground clutter is automatically removed from WSR-88D imagery, so typically it is does not interfere with image interpretation.
Kadar Image from National Weather Service: KCLE 16:46 UTC US/1fZUUS + Saginaw Port Huron + London Findlay oungstown + Manstield Ground Clutter Columbus + Cambridge Zanesville Dayton + New Lexington + Morgantown Fainmont Radar Image from National Weather Service: KCLE 16:46 UTC 05/11/2005 Figure 4-8. WSR-88D Weather Radar Ground Clutter Example Section 4: Radar and Satellite Imagery Page 4-7
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010)
4.1.4.1.3.4 Ghost A Ghost (Figure 4-9) is a diffused echo in apparently clear air caused by a “cloud” of point targets such as insects or by refraction returns of the radar beam in truly clear air.
The latter case commonly develops at sunset due to superrefraction during the warm season.
The ghost develops as an area of low reflectivity echoes (typically less than 15dBZ) near the radar site and quickly expands. When animating the imagery, the ghost echo shows little movement.
Figure 4-9. WSR-88D Weather Radar Ghost Example
4.1.4.1.3.5 Angels Angels are echoes caused by a physical phenomenon not discernible by the eye at the radar site. They are usually caused by bats, birds or insects. Angels typically appear as a donut-shaped echo with low reflectivity values (Figure 4-10). When animated, the echo expands and becomes more diffuse with time.
Angels typically only appear only when the radar is in Clear Air Mode because of their weak reflectivity. Echoes caused by birds are typically detected in the morning when they take flight for the day. Echoes caused by bats are typically detected in the evening, when they are departing from caves.
Section 4: Radar and Satellite Imagery Page 4-8
Aviation Weather Services, Advisory Circular 00-45G, Change 1 (July 2010)
Figure 4-10. WSR-88D Weather Radar Angle Example This angel was caused by bats departing Selman Bat Cave at Alabaster Caverns State Park, Oklahoma around sunset.
4.1.4.1.3.6 Anomalous Propagation (AP) Anomalous propagation (AP) (Figure 4-11) is an en extended pattern of ground echoes caused by superrefraction of the radar beam. Superrefraction causes the radar beam to bend downward and strike the ground. It differs from ground clutter because it can occur anywhere within the radar’s range, not just at ranges close to the radar.
AP typically appears as speckled or blotchy, high reflectivity echoes. When animating images, AP tends to “bloom up” and dissipate and has no continuity of motion. AP can sometimes be misinterpreted as thunderstorms; differentiating between to two is determined by animating images. Thunderstorms move with a smooth, continuous motion while AP appears to “bloom up” and dissipate randomly.
Section 4: Radar and Satellite Imagery Page 4-9