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 | 5,448,819 |
| episode_id | 1,189,557 |
| begin_utc | 2005-04-02T19:00:00+00:00 |
| end_utc | 2005-04-03T08:00:00+00:00 |
| state | NEW JERSEY |
| cz_type | Z |
| cz_name | EASTERN ATLANTIC |
| deaths_direct | 0 |
| deaths_indirect | 0 |
| injuries_direct | 0 |
| injuries_indirect | 0 |
| damage_crops | 0 |
| wfo_source | COASTAL OBSERVING STATION |
| episode_narrative | Strong southeast winds and runoff from the heavy rain in the Delaware River caused minor tidal flooding at the time of the late afternoon and early evening high tide along the Delaware River and Delaware Bay. The same southeast winds caused some minor tidal flooding at the time of the overnight high tide along the Atlantic Coast. The high tide reached 7.9 feet above mean lower low water at Reedy Island (New Castle County). Minor tidal flooding begins at 7.2 feet above mean lower low water. The overnight high tide at Sandy Hook (Monmouth County) reached 6.93 feet above mean lower low water. Minor tidal flooding begins at 6.7 feet above mean lower low water. The minor tidal flooding was caused by the strong southeast winds preceding and accompanying the low pressure system that moved from the southern Gulf Coast States toward the region on the morning of the 2nd. At 7 a.m. EST on the 2nd, the low pressure system was in central Virginia. From Virginia it continued to move northeast and intensified as it neared Washington, D.C. at 1 p.m. EST on the 2nd, Lancaster, Pennsylvania at 7 p.m. EST on the 2nd and Scranton, Pennsylvania at 1 a.m. EST on the 3rd. |
| year | 2,005 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine