The record
Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.
| event_type | Astronomical Low Tide |
|---|---|
| ncei_event_id | 80,100 |
| episode_id | 12,598 |
| begin_utc | 2008-02-11T02:00:00+00:00 |
| end_utc | 2008-02-12T07:00:00+00:00 |
| state | NEW JERSEY |
| cz_type | Z |
| cz_name | CAMDEN |
| deaths_direct | 0 |
| deaths_indirect | 0 |
| injuries_direct | 0 |
| injuries_indirect | 0 |
| damage_property | 0.00K |
| damage_crops | 0.00K |
| wfo_source | C-MAN Station |
| episode_narrative | Persistent and strong west to northwest winds caused blowout tide conditions to occur at times of low tide along the Delaware River and tidal sections of its tributaries from the evening low tide on the 10th through the overnight low tide on the 11th. The lowest tide at Reedy Island (New Castle County) was -2.06 feet below mean lower low water. The lowest tide at Phialdelphia Pier 12 (Philadelphia County) was -1.98 feet below mean lower low water. Blowout tides begin at -1.80 feet below mean lower low water. The persistent west to northwest winds were caused by the pressure gradient (difference) between a high pressure system that was moving east from the Northern Plains and Great Lakes and an intense low pressure system over the Canadian Maritimes. |
| year | 2,008 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine