Record-breaking rainfall extremes are becoming more frequent in a warming climate, particularly intense short-duration events that often lead to pluvial (or flash) flooding in urban areas.[1] This increase can be attributed to the ability of a warmer atmosphere to hold more moisture as well as variations in regional weather patterns.[2] At the same time, urban expansion has occurred at a rapid pace across the world in recent decades. This growth of impervious surfaces, along with inadequate or aging floodwater drainage systems, means that an increasing proportion of the world’s population is at risk of urban flooding.
In 2023, several urban regions around the globe experienced severe flash flooding, with two notable instances being New York City and Hong Kong. These events epitomized the pressing challenges that urban populations face in adapting to climate change. Both cities, each home to around 7 million to 8 million people, saw record-breaking rainfall over a short period that overwhelmed infrastructure and led to questions about their readiness to manage flood risks in a warmer world.[3],[4]
Global extremes: New York City and Hong Kong
In September 2023, New York City was hit by an exceptional rainfall event that resulted in widespread flash flooding. The remnants of Tropical Storm Ophelia merged with a mid-latitude weather system off the northeastern U.S. coastline on September 28. This confluence then stalled over New York City for 12 hours, leading to an extraordinary deluge.
Precipitation totals of over 200 millimeters were recorded at many locations within just a few hours on the morning of September 29. Queens, Kings and Nassau counties were among those recording the highest totals.[5] Notably, John F. Kennedy Airport registered nearly 220 millimeters of rainfall in a single day, surpassing all previous records at the site.[6] Neighboring areas in the states of New Jersey and Connecticut also experienced severe flooding.
In New York City, the flooding disrupted public transportation, with subway and train services suspended and several highways closed. Governor Kathy Hochul declared a state of emergency for five boroughs, and the New York Army National Guard was deployed. The flooding also led to partial roof collapses, inundated basements and overwhelmed sewers. It is now the third time in two years that New York has seen severe pluvial flooding, following the devastating impact of post-tropical cyclone Ida in 2021.[7]
Earlier in the month, Hong Kong experienced a similar situation, when the remnants of Typhoon Haikui stalled over the Pearl River Delta between September 7 and 8. The low-pressure system interacted with the seasonal monsoon, depositing huge amounts of precipitation over Hong Kong and the broader Pearl River Delta area. This event marked the heaviest rainfall recorded in Hong Kong since records began 140 years ago. The Hong Kong Observatory recorded over 600 millimeters of rainfall within 24 hours, with parts of Hong Kong Island receiving over 800 millimeters,[8] far exceeding the city's average September rainfall of around 320 millimeters.
The overall impact of the floods was devastating, with 15 fatalities (four in Hong Kong and 11 in Guangxi). Like New York City, infrastructure was overwhelmed. Shopping malls and underground railway stations were deluged. Landslides also occurred, with large boulders tumbling down roads and causing significant damage. The government declared that the city was under “extreme conditions,” advising employers that nonessential workers should not be required to report for duty.
Urban development and flood risk
Around the world, cities continue to grow in terms of both population and spatial footprint. A recent study led by the World Bank found that between 1985 and 2015, the built-up area across the world grew by 85%, from 693,000 to over 1.28 million square kilometers.[9]
Table 1. Share (%) of global settlements facing various inundation depths during any type (pluvial, fluvial and coastal) of 1-in-100-year flood
| No risk | Low risk (<0.15m) | Medium risk (<0.5m) | High risk (<1.5m) | Very high risk (>1.5m) | Extent of global settlement (km2, millions) | |
|---|---|---|---|---|---|---|
| 1985 | 64.2 | 17.8 | 8.1 | 5.5 | 4.3 | 0.69 |
| 2025 | 64.3 | 17.8 | 8.7 | 6.1 | 5.2 | 1.28 |
| Change | -1.9 | 0 | 0.6 | 0.6 | 0.9 | 0.59 |
At the same time, the proportion of urban areas at low risk of all types of flooding (pluvial, fluvial and coastal) decreased by 1.9 percentage points, while the percentage of settlements in areas classified as high or very high flood risk increased (Table 1).
This urban expansion in high-risk flood zones is being largely driven by developing nations, particularly in East Asia, where the rate of growth in areas susceptible to flooding is 60% faster than in areas with lower flood risks. In many cities, such as Da Nang in Vietnam, this growth is being fueled by construction on land that has been reclaimed from waterways or the sea.
Urban expansion is only part of the story, however, with inadequate or aging drainage also playing a role. Take New York City as an example: Like many major cities, it has a stormwater drainage system built to manage only moderate-intensity rainfall events. The city's standard design criterion is aligned with a storm that has a five-year return period, equating to 44 millimeters per hour.[10]








