| 1946 Pacific typhoon season | |
|---|---|
 Season summary map | |
| Seasonal boundaries | |
| First system formed | March 27, 1946 |
| Last system dissipated | November 20, 1946 |
| Strongest storm | |
| Name | Lilly |
| • Maximum winds | 220 km/h (140 mph) (1-minute sustained) |
| • Lowest pressure | 927 hPa (mbar) |
| Seasonal statistics | |
| Total storms | 19 |
| Typhoons | 18 |
| Super typhoons | 0 (unofficial) |
| Total fatalities | Unknown |
| Total damage | Unknown |
| Related articles | |
The 1946 Pacific typhoon season has no official bounds; it ran year-round in 1946, but most tropical cyclones tend to form in the northwestern Pacific Ocean between June and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.
The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the date line and north of the equator are called hurricanes; see 1946 Pacific hurricane season. At the time, tropical storms that formed within this region of the western Pacific were identified and named by the United States Armed Services, and these names are taken from the list that USAS publicly adopted before the 1945 season started.[1][2]
- ^ Landsea, Christopher W; Dorst, Neal M (June 1, 2014). "Subject: Tropical Cyclone Names: B1) How are tropical cyclones named?". Tropical Cyclone Frequently Asked Question. United States National Oceanic and Atmospheric Administration's Hurricane Research Division. Archived from the original on December 10, 2018.
- ^ Cry, George (July 1958). Bristow, Gerald C (ed.). "Naming hurricanes and typhoons". Mariners Weather Log. 2 (4): 109. hdl:2027/uc1.b3876059. ISSN 0025-3367. OCLC 648466886.