Satellite Cloud Product
NESDIS produces a Satellite Cloud Product (SCP) that supplements the ASOS ceilometer readings. This page merges the SCP data with the METAR observations for a given UTC date. Cloud level values are presented in feet above ground level. ECA represents estimated cloud amount expressed in percentage. An IEM Web Service provided the following JSON dataset for this page. Data is available for some sites back to 1993.
| SCP Valid UTC | METAR Valid Local | Satellite East Sounder | Satellite West Sounder | ASOS METAR Report | |||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Mid Clouds | High Clouds | Levels [ft] | ECA [%] | Mid Clouds | High Clouds | Levels [ft] | ECA [%] | Levels ft | METAR | ||
| 0550Z | 12:53 AM | SCT | 13000 - 43000 | 13 | SCT | 13000 - 42000 | 14 | CLR | KDWH 030553Z AUTO 04005KT 10SM CLR 24/23 A2995 RMK AO2 SLP138 60000 T02440228 10256 20244 58003 | ||
| 0650Z | 1:53 AM | SCT | 13000 - 30000 | 13 | SCT | 13000 - 41000 | 12 | CLR | KDWH 030653Z AUTO 06004KT 8SM CLR 24/23 A2994 RMK AO2 SLP135 T02390233 | ||
| 0750Z | 2:53 AM | SCT | 13000 - 47000 | 3 | SCT | 13000 - 38000 | 3 | CLR | KDWH 030753Z AUTO 05004KT 6SM BR CLR 24/23 A2993 RMK AO2 SLP132 T02390233 | ||
| 0850Z | 3:53 AM | SCT | 13000 - 39000 | 3 | SCT | 13000 - 39000 | 5 | CLR | KDWH 030853Z AUTO 36004KT 6SM BR CLR 24/23 A2992 RMK AO2 SLP130 T02390233 56007 | ||
| 0950Z | 4:53 AM | SCT | 19000 - 45000 | 0 | SCT | SCT | 13000 - 41000 | 3 | CLR | KDWH 030953Z AUTO 03004KT 7SM CLR 24/23 A2991 RMK AO2 SLP127 T02390233 | |
| 1050Z | 5:53 AM | SCT | 13000 - 49000 | 20 | BKN | 13000 - 43000 | 26 | CLR | KDWH 031053Z AUTO 01003KT 6SM BR CLR 24/23 A2993 RMK AO2 SLP131 T02390233 | ||
| 1150Z | 6:53 AM | SCT | 13000 - 50000 | 12 | SCT | 13000 - 46000 | 14 | CLR | KDWH 031153Z AUTO 03004KT 6SM BR CLR 24/23 A2993 RMK AO2 SLP133 70088 T02390233 10244 20239 53003 | ||
| 1250Z | 7:53 AM | BKN | 29000 - 52000 | 49 | BKN | 14000 - 52000 | 46 | CLR | KDWH 031253Z 36003KT 5SM BR CLR 24/23 A2995 RMK AO2 SLP140 T02390233 | ||
| 1350Z | 8:53 AM | BKN | 13000 - 52000 | 42 | BKN | 14000 - 46000 | 45 | SCT@900 | KDWH 031353Z VRB03KT 7SM SCT009 25/24 A2997 RMK AO2 SLP146 T02500239 | ||
| 1450Z | 9:53 AM | SCT | 13000 - 49000 | 21 | BKN | 13000 - 41000 | 30 | SCT@1000 BKN@11000 | KDWH 031453Z 03007KT 8SM SCT010 BKN110 26/24 A2997 RMK AO2 SLP147 T02610239 51014 | ||
| 1550Z | 10:49 AM | SCT | 13000 - 46000 | 23 | SCT | 13000 - 44000 | 21 | SCT@1700 | KDWH 031549Z 08007KT 9SM SCT017 28/24 A2998 RMK AO2 | ||
| 1650Z | 11:48 AM | BKN | 13000 - 52000 | 29 | SCT | 13000 - 43000 | 22 | SCT@2300 BKN@3100 | KDWH 031648Z 04007KT 010V080 9SM SCT023 BKN031 29/24 A2997 RMK AO2 | ||
| 1750Z | 12:53 PM | BKN | 13000 - 51000 | 33 | BKN | 13000 - 44000 | 38 | BKN@3200 BKN@4300 BKN@5500 | KDWH 031753Z 05007KT 10SM BKN032 BKN043 BKN055 31/24 A2995 RMK AO2 SLP140 T03110239 10311 20239 58009 | ||
| 1850Z | 1:53 PM | BKN | 13000 - 49000 | 36 | BKN | 13000 - 42000 | 43 | SCT@3000 BKN@3800 BKN@6500 | KDWH 031853Z 06006KT 10SM SCT030 BKN038 BKN065 30/23 A2993 RMK AO2 RAB39E48 SLP132 P0000 T03000233 | ||
| 1950Z | 2:53 PM | BKN | 13000 - 41000 | 59 | BKN | 13000 - 41000 | 56 | SCT@3000 BKN@7500 | KDWH 031953Z 04006KT 10SM SCT030 BKN075 31/23 A2990 RMK AO2 SLP123 T03060233 | ||
| 2050Z | 3:53 PM | BKN | 13000 - 49000 | 51 | BKN | 13000 - 38000 | 49 | SCT@3000 BKN@9500 | KDWH 032053Z 06008KT 10SM SCT030 BKN095 31/23 A2989 RMK AO2 SLP118 60000 T03060228 56021 | ||
| 2150Z | 4:53 PM | BKN | 13000 - 47000 | 42 | BKN | 13000 - 43000 | 37 | BKN@3600 BKN@5000 OVC@7000 | KDWH 032153Z 04009G18KT 5SM RA BKN036 BKN050 OVC070 28/24 A2990 RMK AO2 RAB51 SLP122 P0002 T02780239 | ||
| 2250Z | 5:53 PM | BKN | 13000 - 39000 | 57 | BKN | 14000 - 43000 | 54 | BKN@4000 OVC@8500 | KDWH 032253Z 35007KT 10SM -RA BKN040 OVC085 27/24 A2990 RMK AO2 RAE16B37 SLP123 T02670239 PNO $ | ||
| 2350Z | 6:53 PM | OVC | 20000 - 44000 | 66 | OVC | 22000 - 42000 | 67 | FEW@2500 SCT@11000 | KDWH 032353Z VRB04KT 9SM FEW025 SCT110 26/24 A2992 RMK AO2 LTG DSNT N RAE31 SLP130 6//// T02560239 10311 20256 53011 PNO $ | ||