The record
Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.
| event_type | Storm Surge/Tide |
|---|---|
| ncei_event_id | 5,328,705 |
| episode_id | 1,165,066 |
| begin_utc | 2003-12-14T19:00:00+00:00 |
| end_utc | 2003-12-15T02:00:00+00:00 |
| state | NEW JERSEY |
| cz_type | Z |
| cz_name | SALEM |
| deaths_direct | 0 |
| deaths_indirect | 0 |
| injuries_direct | 0 |
| injuries_indirect | 0 |
| damage_crops | 0 |
| wfo_source | AWOS,ASOS,MESONET,ETC |
| episode_narrative | The circulation around a low pressure system moving northeast along the Eastern Seaboard and a high pressure system which begrudgingly moved away from New England produced onshore flow during the day on the 14th. This led to minor tidal flooding along tidal sections of the Delaware River and its tributaries during the late afternoon and early evening of the 14th. The high tide in Burlington reached 10.35 feet above mean lower low water. Minor tidal flooding starts at 9.0 feet above mean lower low water. The high tide in Philadelphia reached 9.00 feet above mean lower low water. Minor tidal flooding starts in Philadelphia at 8.2 feet above mean lower low water. The high tide at Reedy Island (Delaware) reached 7.49 feet above mean lower low water. Minor flooding at Reedy Island starts at 7.2 feet above mean lower low water. The low pressure system responsible for the tidal flooding developed in the Gulf of Mexico on the 13th and moved northeast reaching the Alabama coastal waters on the evening of the 13th, the southern North Carolina coast the morning of the 14th, near Norfolk during the early afternoon of the 14th, crossed Delaware Bay during the early evening of the 14th and crossed across coastal New Jersey during the rest of the evening of the 14th. |
| year | 2,003 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine