Hilo — The Wettest City in America, Rebuilt Twice, and Genuinely Local
Hilo is the county seat and largest town on the island of Hawaii -- the "Big Island" -- sitting on Hilo Bay at the base of Mauna Kea on the island's windward, rainy east side. It is, by a wide and well-documented margin, the wettest city in the United States: roughly 126 to 130 inches of rain fall on the town itself in an average year, and the foothills just a few miles upslope receive closer to 200 to 300 inches. That rainfall built the town's identity as much as anything else -- lush, green, agricultural, and genuinely local in a way the drier, resort-heavy Kona side of the island is not. Hilo is also, without question, the most tsunami-devastated town in modern American history. An April 1, 1946 tsunami, generated by a magnitude 8.6 earthquake in the Aleutian Islands, sent waves as high as 32 to 37 feet over Hilo's harbor breakwater and killed 96 people in Hilo alone (159 statewide) -- and a second tsunami, on May 23, 1960, generated by the magnitude 9.5 earthquake off Chile (the largest earthquake ever recorded on modern instruments), killed 61 more people in Hilo and destroyed or damaged more than 500 homes and businesses. Both disasters are the direct reason the Pacific Tsunami Warning Center exists today, and both are the direct reason a wide belt of Hilo's original bayfront commercial and residential district -- including the historically Japanese-American Shinmachi neighborhood -- was never rebuilt as private property and instead became the parkland that still separates downtown Hilo from the water. This page treats that history factually and soberly, because it is not background trivia -- it is the single most important fact shaping how modern Hilo is laid out, insured, and built. Where this research could not independently confirm a figure -- an exact current short-term-rental property tax rate, a Hilo-specific homeowner insurance premium, or a precise leasehold share of the local housing stock -- this page says so rather than guessing.
What Actually Makes Hilo Different
Hilo is not a resort town, and it is not trying to be one. It is Hawaii County's seat of government, the Big Island's largest population center, and a genuinely local, working town built around a working harbor, a state university, and an agricultural economy that predates tourism by more than a century. That character is a direct, deliberate contrast with the island's other major population center, Kailua-Kona, on the dry, sunny, resort-lined leeward side: island brokerages and travel writers consistently describe Hilo as the more affordable, less touristy, more distinctly local option, with a 1950s-era downtown of intact plantation-period storefronts, a university population from the University of Hawaii at Hilo (roughly 2,668 students as of fall 2024, on a 115-acre campus), and a Wednesday-through-Saturday farmers market culture that draws longtime residents rather than tour buses. Home prices reflect that split -- Hilo's median sale price has clustered somewhere in the roughly $480,000-to-$660,000 range across various 2025-2026 market snapshots (sources genuinely disagree on the exact figure and trend direction in this small market), while Kailua-Kona's median has run meaningfully higher, from roughly $675,000 to well above $800,000 depending on the source and month. Treat both ranges as directional, not settled, but the gap between the two towns is real and repeatedly documented.
The rain is not incidental to any of this -- it is close to the whole explanation. Hilo receives roughly 126 to 130 inches of rainfall a year near the bay, and that figure climbs toward 200 to 300 inches a few miles upslope, making it one of the wettest inhabited places in the entire United States by a wide margin, cited across multiple independent climate sources as the wettest major American city outright. That rainfall is why the Big Island's macadamia nut industry -- the first Hawaii macadamia plantation was established in Hilo in 1921, and Castle & Cooke's 1,000-acre orchard near Keaau (just outside Hilo), planted in 1949, grew into what became the Mauna Loa Macadamia Nut Corporation -- and its tropical-flower and orchid trade both took root here rather than on the drier Kona side. It's also why Hilo is green in a way few American towns are: waterfalls inside the town limits, rainforest a short drive upslope, and a genuinely different visual and sensory experience than the sunbaked resort corridor most visitors picture when they think of Hawaii. Hilo also functions as the real, practical gateway to Hawaii Volcanoes National Park, roughly 30 miles and about 45 minutes south via Highway 11 -- closer to the park than any other town of comparable size on the island.
None of that changes the fact that this is, first and foremost, the most tsunami-devastated town in documented US history, and any honest guide to Hilo has to lead with that rather than bury it. On April 1, 1946, a magnitude 8.6 earthquake in the Aleutian Islands sent a tsunami racing across the Pacific that struck Hilo with waves reported as high as 32 to 37 feet, overtopping the town's harbor breakwater -- a structure completed in 1929 specifically to calm the harbor for shipping, never designed as a tsunami barrier -- and killing 96 people in Hilo alone, out of 159 deaths statewide, while causing an estimated $26 million in damage in 1946 dollars and nearly demolishing the bayfront business district. Fourteen years later, on May 23, 1960, a tsunami generated by the magnitude 9.5 earthquake that struck Chile the day before -- still, as of this writing, the largest earthquake ever recorded on modern seismographic instruments -- arrived in Hilo as a series of waves, the largest reported near 35 feet, that killed 61 people, injured 282 more, and destroyed or damaged over 500 homes and businesses, this despite a Pacific-wide warning that reached Hawaii many hours ahead of the waves. Both disasters together are the direct reason the Pacific Tsunami Warning Center exists (its predecessor, the Seismic Sea Wave Warning System, was established in 1949 specifically in response to the 1946 disaster) and the direct reason the historically Japanese-American Shinmachi neighborhood along the bayfront, along with much of the rest of the original downtown waterfront district, was never rebuilt as private housing or commerce after 1960 -- it became Wailoa River State Recreation Area, Liliuokalani Gardens, and the wide belt of public parkland that still, today, physically separates rebuilt downtown Hilo from Hilo Bay. That green space is not decorative landscaping; it is the visible, permanent legacy of two mass-casualty disasters, and it shapes where a buyer can and cannot build today.
Hilo today runs on a mature, actively maintained tsunami warning and evacuation infrastructure that exists because of that history: a statewide monthly siren test on the first business day of each month, official tsunami evacuation zone maps published by Hawaii County Civil Defense covering every foot of the bayfront and low-lying downtown, and the Pacific Tsunami Warning Center itself, which -- worth stating precisely rather than loosely -- is headquartered at Ewa Beach on Oahu, not in Hilo, even though Hilo's own Pacific Tsunami Museum, housed in a downtown building that itself survived both disasters, exists specifically to preserve this history and educate residents and visitors on tsunami science and preparedness. Hawaii's real property ownership landscape adds one more layer worth understanding before shopping here: most Big Island property, including most of Hilo, is sold fee simple (outright ownership of land and structure), but leasehold arrangements -- where a buyer owns the structure but leases the underlying land on a long-term ground lease, often from large historic landowners -- do exist here, particularly in some older and agricultural-zoned subdivisions, and the distinction meaningfully affects financing, resale, and long-term cost. This page's sub-pages on property tax, buying process, flood zones, and coastal insurance each go deeper into these specifics with real, sourced figures, and flag plainly where this research could not confirm a number rather than inventing one.
Independent research. No ads. No sponsored listings. Facts here are drawn from: NOAA and the International Tsunami Information Center / UNESCO IOC Tsunami Programme for the April 1, 1946 Aleutian Islands earthquake and tsunami details; Hawaii News Now, Big Island Now, the National Library of Medicine's "Native Voices" timeline, and EarthMagazine's retrospective for the 1946 Hilo death toll (96 in Hilo, 159 statewide), wave heights, and $26 million damage estimate; the Britannica and History.com entries on the 1960 Chile earthquake, the Moody's/WSSPC/USGS tsunami retrospectives, and usdeadlyevents.com's sourced casualty compilation for the May 23, 1960 Hilo death toll (61 killed, 282 injured) and the M9.5 Chile earthquake's status as the largest instrumentally recorded earthquake; Hawaii Sea Grant, HAWAI'I Magazine, and Hive/community history writing on the Shinmachi neighborhood's conversion to Wailoa River State Recreation Area and Liliuokalani Gardens after 1960; the tsunami.gov (Pacific Tsunami Warning Center) official history page and the NLM timeline for the 1949 founding of the Seismic Sea Wave Warning System and PTWC's current Ewa Beach, Oahu headquarters; imagesofoldhawaii.com and University of Hawaii at Hilo student research (Hohonu journal) for the Hilo breakwater's 1908-1929 construction timeline and its role in the 1946 disaster; the National Weather Service, Hawaii News Now, and UH Hilo's own natural-hazards program page for Hurricane/Tropical Storm Iselle's August 8, 2014 landfall, damage, and power-outage figures; the USGS Hawaiian Volcano Observatory for the island's Lava Flow Hazard Zone system and the 1881 Mauna Loa flow's approach to Hilo; the U.S. Census Bureau (2020 Census) for Hilo CDP's population, with a 2024 demographic-aggregator estimate (Hawaii-Demographics/World Population Review, not an official Census release) flagged as such; the University of Hawaii at Hilo's own enrollment data page for fall 2024 figures; the Merrie Monarch Festival's own official history page for its 1964 founding and connection to King Kalakaua; the Hawaii Department of Taxation and Hawaii County Finance Department for current GET, state TAT, and county TAT rates; Hawaii County Council Resolution 574-26 and multiple 2025-2026 property-tax explainer sites (howtoliveinhawaii.com, propertytaxrates.org) for FY2026-27 real property tax classifications and rates; and Redfin, Zillow, and Realtor.com market snapshots for home price ranges, explicitly flagged here as disagreeing with each other in this small, thin market. Facts not independently confirmed and not invented here include: a specific short-term-rental-only property tax classification rate distinct from the non-owner-occupied tiers; the exact current percentage of Hilo's housing stock that is leasehold versus fee simple; and a parcel-specific lava hazard zone number for any individual address. Confirm all current facts directly with Hawaii County's Real Property Tax Division, Hawaii County Civil Defense Agency, a licensed Hawaii insurance professional, and a local buyer's agent before making a purchase, relocation, or investment decision. Nothing on this page is legal, tax, financial, insurance, or emergency-management advice.