The Pacific Torrent: !!top!!

| Year | Duration (days) | Max daily precip (mm) | Total precip (mm) | Primary driver | Damages (2024 USD) | |------|----------------|------------------------|------------------|----------------|--------------------| | 1955 | 18 | 410 | 3,820 | Strong El Niño + warm blob | $5.2B (mostly agricultural) | | 1983 | 16 | 380 | 3,450 | Extreme El Niño | $8.1B | | 1997 | 19 | 520 | 4,110 | Super El Niño + Pacific Decadal Oscillation positive | $14.3B | | 2023 | 15 | 470 | 3,900 | El Niño + marine heatwave | $11.0B |

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Ralph et al. (2017) defined ARs as narrow corridors of strong horizontal water vapor transport. However, most studies focus on 24–72 hr events. Dettinger (2013) noted “AR families”—repeated landfalls over 7–10 days—but did not define thresholds for a single continuous torrent. Paleoflood evidence from the Sacramento Valley (Ingram & Malamud-Roam, 2013) indicates “megafloods” with 45-day durations in the 9th, 14th, and 17th centuries, likely caused by persistent PTs under specific sea surface temperature (SST) anomalies. the pacific torrent

No previous work has explicitly compared the physics of sustained water vapor transport to the economics of sustained capital/cultural transport. This paper builds an analogy based on three shared properties: (1) (warm pool / industrial East Asia), (2) corridor (subtropical jet stream / shipping lanes and fiber-optic cables), and (3) orographic lift / regulatory friction (coastal mountains / tariffs and content regulations). 3. Methods 3.1 Defining the Physical Pacific Torrent | Year | Duration (days) | Max daily

| Decade | Two-way Pacific trade (US-East Asia, $B) | Korean/Japanese content on US streaming (%) | Patent cross-citations (%) | |--------|-------------------------------------------|-----------------------------------------------|----------------------------| | 1970 | 40 | <0.1 | 2 | | 1985 | 120 | 0.5 | 5 | | 2000 | 620 | 3 | 12 | | 2010 | 1,100 | 8 | 19 | | 2025 | 2,480 | 27 | 31 | However, most studies focus on 24–72 hr events

We compare the cumulative distribution function (CDF) of precipitation in PT events with the CDF of trade growth across the Pacific, using normalized units. A Kolmogorov–Smirnov test checks distribution similarity. 4.1 Historical Physical Pacific Torrents (1948–2024)