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Extreme heat warning

An extreme heat warning is an official alert issued by meteorological and public health authorities to inform the public of imminent or ongoing periods of dangerously high temperatures and humidity that threaten human health, prompting immediate protective actions to prevent heat-related illnesses and deaths. These warnings are part of broader heat health early warning systems (HHEWS) designed to reduce morbidity and mortality by raising awareness and enabling timely responses, such as staying hydrated, seeking air-conditioned environments, and limiting outdoor exertion. In the United States, the (NWS) issues an Extreme Heat Warning—renamed from Excessive Heat Warning in March 2025—when local criteria for extreme danger are met, typically a (a combined measure of and ) of at least 105°F (41°C) for more than three hours per day over two consecutive days, or 110°F (43°C) for any duration, though thresholds vary by region to account for and vulnerability. The warning is declared 12 to 24 hours in advance of the event or during its occurrence, often alongside an Extreme Heat Watch issued 24 to 72 hours prior when conditions are favorable. Internationally, similar systems operate under frameworks like those recommended by the , with many countries implementing HHEWS tailored to local climates, such as Europe's Meteoalarm network or Australia's alerts, which use impact-based thresholds to forecast risks to vulnerable populations including the elderly, children, and outdoor workers. Extreme heat events necessitating these warnings represent the deadliest weather-related hazard globally, causing approximately 489,000 deaths annually between 2000 and 2019, with and accounting for over 80% of cases, often exacerbated by urban heat islands and . In the , extreme heat claims an average of 702 lives each year (2004–2018), surpassing fatalities from floods, tornadoes, and hurricanes combined, highlighting the warnings' role in saving lives through public education and emergency preparedness. As global temperatures rise, the frequency and intensity of these events are increasing, underscoring the need for enhanced warning systems integrated with climate adaptation strategies.

Overview

Definition

An extreme heat warning is a severe weather alert issued by meteorological agencies, such as the U.S. National Weather Service (NWS), when conditions are expected to meet local criteria for extreme heat danger, typically involving a heat index (a measure combining temperature and humidity) of at least 105°F (41°C) for more than three hours per day for two or more consecutive days, or a heat index of 110–115°F (43–46°C) for any duration, though exact thresholds vary by region to reflect local acclimatization and vulnerabilities. This alert signifies the highest level of heat danger, surpassing heat advisories and watches, and is designed to communicate the urgent need for protective measures during periods of prolonged or intense high temperatures combined with humidity. The primary purpose of an extreme heat warning is to alert the public to conditions that can cause heat-related illnesses, such as and heatstroke, and potentially lead to fatalities, thereby encouraging immediate actions like seeking air-conditioned spaces and limiting outdoor exertion. By providing timely notifications, these warnings aim to reduce health impacts in communities exposed to such hazards, particularly during exacerbated by . Key components of an extreme heat warning include specifications on the expected duration and geographic areas affected, along with basic safety recommendations integrated into the alert message, such as staying hydrated and avoiding strenuous activities. These alerts are disseminated through official channels like the and local media to ensure broad reach. On March 4, 2025, the NWS renamed the previous "Excessive Heat Warning" to "Extreme Heat Warning" as part of its Hazard Simplification Project, following evaluations including a 2018 public survey that highlighted the need for terminology emphasizing the severity of risks to improve public comprehension and response.

History and Evolution

The origins of extreme heat warnings in the United States date to the early , when devastating exposed the need for public alerts amid limited forecasting capabilities. The , exacerbated by drought and poor soil management, caused over 5,000 deaths across the Midwest and Plains states, prompting the U.S. Weather Bureau—the NWS predecessor—to issue initial informal heat forecasts and advisories through newspapers and local broadcasts to urge precautions like seeking shade and hydration. Key milestones in the formalization of these warnings emerged in the late . The NWS adopted the in 1979, a developed by Robert G. Steadman to quantify the physiological stress from combined high temperatures and humidity, providing a scientific basis for . Building on this, the NWS introduced standardized Excessive Heat Warnings in the , following mid-decade research that refined criteria to account for regional vulnerabilities and nighttime temperatures, marking a shift from ad hoc alerts to proactive, nationwide protocols. By the 2000s, these systems expanded with the integration into broader frameworks, including the rollout of Heat-Health Warning Systems in over 20 U.S. metropolitan areas by 2007 to link meteorological data with coordination. Parallel developments occurred globally, particularly in Europe after the 2003 heat wave that killed about 70,000 people, primarily from heat-related illnesses in urban areas. This catastrophe accelerated the creation of early warning systems, such as the UK's Heat-Health Alert framework launched in 2004, which uses a tiered alert structure (yellow, amber, red) to trigger targeted interventions like cooling centers and health service escalations.

Issuance Process

Criteria for Issuance

The (NWS) issues an Extreme Heat Warning (formerly known as an Excessive Heat Warning)—commonly referred to as an extreme heat warning—when forecast conditions meet specific thresholds indicating dangerous heat stress, primarily based on the , which accounts for the combined effects of and humidity on the . In March 2025, the NWS renamed the Excessive Heat Warning to Extreme Heat Warning to enhance clarity in public messaging. The standard national criteria require a heat index of at least 105°F (41°C) for more than three hours per day over at least two consecutive days, or a heat index of 115°F (46°C) or higher at any time, with warnings typically issued when these conditions are expected within 12 to 24 hours. These thresholds are designed to signal widespread risk of heat-related illnesses, and local NWS offices may adjust them based on regional climate acclimation and historical impacts. The heat index is calculated using a formula developed by the NWS to estimate apparent temperature, incorporating air temperature (T in °F) and relative humidity (RH in percent): \text{HI} = -42.379 + 2.04901523T + 10.14333127\text{RH} - 0.22475541T \cdot \text{RH} - 6.83783 \times 10^{-3}T^2 - 5.481717 \times 10^{-2}\text{RH}^2 + 1.22874 \times 10^{-3}T^2 \cdot \text{RH} + 8.5282 \times 10^{-4}T \cdot \text{RH}^2 - 1.99 \times 10^{-6}T^2 \cdot \text{RH}^2 This equation, derived from a multi-regression model of human heat perception studies, applies primarily to shaded conditions at low wind speeds and is adjusted for direct sunlight or higher winds in operational use. For temperatures below 80°F or humidity above 85%, simplified adjustments are applied to avoid overestimation. Regional NWS offices tailor criteria to local conditions, recognizing that acclimation and environmental factors influence heat vulnerability. In the arid Southwest deserts, such as around , where low humidity reduces the 's relevance, warnings often focus on dry-bulb air temperature thresholds, such as daytime highs of 110°F (43°C) or more for at least two consecutive days, supplemented by the HeatRisk tool that integrates temperature, duration, and overnight recovery. In contrast, the humid Southeast, including areas like and , typically maintains or slightly elevates heat index thresholds—such as 108–112°F (42–44°C) for warnings—due to higher population acclimation to steamy conditions, ensuring alerts align with elevated health risks from muggier air. These variations are informed by ongoing assessments of local heat event outcomes. The issuance process begins with models, including the North American Mesoscale () model, which provides high-resolution forecasts of temperature and up to 84 hours ahead, combined with global models like the Global Forecast System (GFS) for longer-range guidance. Forecasters at local NWS offices analyze these outputs alongside observational data from weather stations and satellites to project values, then coordinate with state and local agencies to confirm impacts and public response readiness. Warnings are issued with a of 24 to when confidence exceeds 80%, allowing time for protective actions. Post-issuance, the NWS conducts through event reviews and assessments, comparing forecasted conditions against observed to evaluate accuracy and refine criteria based on actual , , and environmental impacts. For instance, analyses of heat s from 2010–2019 have led to updates like the 2021 HeatRisk tool, which better incorporates acclimation and vulnerability factors to improve future thresholds. Extreme heat warnings differ from heat advisories primarily in severity and immediacy of threat. A heat advisory is issued when conditions pose a significant but not life-threatening risk, typically for values between 100°F and 104°F (38°C to 40°C) persisting over two or more days, or between 105°F and 109°F (41°C to 43°C) for at least three hours in a single day, emphasizing caution and preventive measures like and limiting outdoor exertion. In contrast, an extreme heat warning signals imminent or ongoing extremely dangerous conditions, with values meeting or exceeding 105°F (41°C) for more than three hours per day over two consecutive days, or 115°F (46°C) or higher at any time, where prolonged exposure can lead to severe heat-related illnesses requiring urgent protective actions such as avoiding all outdoor activities. Unlike an excessive heat outlook, which provides a probabilistic long-range forecast of potential 3 to 7 days in advance to allow for planning, an is a short-term issued within 12 to 24 hours of the onset, focusing on immediate response rather than anticipation. Extreme warnings also stand apart from other warnings, such as those for tornadoes or severe storms, as they address non-convective, sustained over hours or days rather than sudden, convective events demanding rapid evacuation or sheltering. No evacuation is typically required for warnings; instead, responses center on staying indoors, using cooling centers, and vulnerable individuals. Within alert systems, heat advisories can escalate to extreme heat warnings if forecasted conditions intensify, creating a tiered for escalating urgency. Internationally, equivalents like Australia's extreme heat warnings under the Australian Warning System employ similar tiering—ranging from advice to levels—to communicate escalating risks based on heat severity and duration.

Health and Environmental Risks

Human Health Dangers

Extreme heat warnings signal conditions that pose severe risks to human health, primarily through heat-related illnesses that overwhelm the body's ability to regulate temperature. These dangers arise when ambient temperatures, often combined with high , exceed the physiological limits of , leading to a of acute effects. The most critical conditions include and , which can progress rapidly if not addressed. Heat stroke represents the most severe form of heat-related illness, characterized by a core body temperature exceeding 104°F (40°C), resulting from the failure of the body's cooling mechanisms. Symptoms include confusion, seizures, and potential death if untreated, as the elevated temperature causes cellular damage and multi-organ dysfunction. , a precursor condition, manifests with symptoms such as , , and a rapid pulse, often due to excessive fluid and loss from sweating. These illnesses impair , where the normally maintains core temperature through sweating and ; under extreme heat, this process falters, leading to . exacerbates the issue by reducing blood volume, which can precipitate organ failure, while high humidity hinders sweat evaporation—the primary method of heat dissipation—trapping moisture on the skin and intensifying heat retention. In the short term, extreme heat imposes significant cardiovascular strain by increasing and to support skin blood flow for cooling, which can trigger heart attacks, arrhythmias, or in susceptible individuals. Respiratory issues also arise, as heat stress worsens breathing difficulties and exacerbates conditions like through dehydration of airways and reduced function. In the United States, extreme heat contributes to approximately 1,220 deaths annually, based on underlying or contributing causes listed on death certificates. In , the US saw a record high of more than 2,300 heat-related deaths, reflecting increasing frequency. Globally, heat-related deaths are estimated at around 489,000 per year (2000–2019), underscoring the widespread immediate threat during extreme heat events.

Impacts on Vulnerable Populations

Extreme heat warnings pose heightened risks to specific demographic and socioeconomic groups due to physiological vulnerabilities and limited access to protective resources. Older adults, particularly those aged 65 and above, experience reduced sweating efficiency and impaired , making them less able to dissipate heat during prolonged exposure. Children and infants, with their higher metabolic rates and lower relative to volume, generate and retain more internal heat, increasing susceptibility to and . Outdoor workers, such as agricultural laborers and construction crews, face prolonged direct exposure to intense sunlight and high temperatures, often without adequate breaks or hydration, elevating risks of and occupational injuries. Similarly, individuals experiencing encounter barriers like limited access to air-conditioned spaces and potable water, exacerbating heat-related illnesses during warnings. Socioeconomic factors further amplify these disparities, as low-income communities often reside in poorly insulated housing without , trapping heat and prolonging exposure. Urban heat islands, where concrete and absorb and radiate heat, can make city neighborhoods up to 10°F (5.5°C) warmer than surrounding rural areas, disproportionately affecting densely populated, lower-income zones. These environmental inequities compound vulnerabilities for marginalized groups, including racial and ethnic minorities. In the United States, studies indicate that and populations face 2-3 times higher -related mortality rates compared to white populations, driven by factors like residential and occupational exposure. Globally, extreme exposure affects billions, with the estimating 1.2 billion at high risk from hazards including heatwaves as of 2024. Indirect consequences include strain, such as heightened anxiety and disruption from stress, which can worsen existing conditions. During the 2023 U.S. , -related calls surged by approximately 30% in affected areas like , overwhelming response systems.

Mitigation and Response

Preparation Strategies

Individuals preparing for extreme heat warnings should prioritize by drinking plenty of fluids throughout the day, even if not feeling thirsty, while avoiding , , and high-sugar beverages that can exacerbate . Wearing lightweight, loose-fitting, light-colored clothing helps reflect and promote air circulation around the body. To minimize exposure, individuals can schedule outdoor activities or strenuous tasks for cooler times, such as early morning or late evening, and seek air-conditioned environments like homes or public cooling centers whenever possible. Home preparation involves simple modifications to reduce indoor temperatures, such as installing shades, reflectors, or drapes to block , weather-stripping and s for better , and using fans or attic ventilators to circulate air. Residents should also check on neighbors, especially older adults and those with chronic conditions, to ensure their . Stocking non-perishable foods, at least one of per person per day, and other essentials in an emergency kit prepares for potential power outages that could disable cooling systems. At the community level, schools and workplaces can develop heat safety plans that include regular hydration breaks, shaded rest areas, and acclimatization schedules allowing new or returning workers to gradually increase exposure over 7-14 days. The World Health Organization and World Meteorological Organization's 2025 guidance emphasizes protections for outdoor workers, including rest breaks and hydration to mitigate heat stress risks. Public awareness efforts, such as the National Weather Service's heat safety resources and OSHA's Heat Illness Prevention Campaign, educate residents on proactive steps like identifying local cooling centers and monitoring vulnerable groups. Useful tools for preparation include mobile applications like the FEMA App, which delivers real-time alerts and emergency notifications, enabling timely adjustments to plans. The NOAA/CDC HeatRisk tool, available since 2023 and updated ongoing, provides location-specific heat risk forecasts to help individuals assess daily threats and plan accordingly. The CDC's Heat and Health Initiative, launched in 2024, promotes actions to stay cool, hydrated, and aware of symptoms. Emergency kits should incorporate replacement packets or sports drinks to support hydration during prolonged heat, alongside basic supplies like water and non-perishables. The U.S. National Heat Strategy (2024-2030) outlines broader efforts to build heat resilience through planning and capacity building.

Response Measures

During an extreme heat warning, individuals are advised to limit strenuous outdoor activities, particularly between noon and 4 p.m., when temperatures peak, to reduce the risk of -related illnesses. Seeking air-conditioned environments, such as homes, malls, or libraries, is recommended to , while staying hydrated with and avoiding or caffeine helps maintain body temperature regulation. People should monitor for symptoms of or , including , , rapid heartbeat, or , and call emergency services immediately if severe signs appear; for , first aid includes moving the person to a cool area, applying cool wet cloths to the skin, and fanning to promote until professional help arrives. Local governments activate cooling centers—such as community centers, libraries, and recreation facilities—during extreme heat warnings to provide free, accessible relief from high temperatures, often extending hours and offering water and snacks. Hospitals prepare for potential surges in heat-related cases by stocking intravenous fluids for dehydration treatment, implementing rapid cooling protocols like cold saline infusions and ice packs, and coordinating with emergency services to manage increased patient loads. Following the event, authorities conduct damage assessments for heat-stressed , including power grids that may experience overloads or failures from heightened for , leading to outages that exacerbate risks. Public health agencies perform surveillance to track spikes in heat-related illnesses, using systems like data and syndromic reporting to evaluate impacts and inform future responses. For multi-day events, response coordination integrates federal support through the (FEMA), which provides technical assistance and resources to states and localities, though full disaster declarations for heat events remain rare due to limited infrastructure damage criteria. In the 2021 , state emergency management offices led coordination with local health departments and activations, highlighting the need for enhanced federal integration in prolonged heat crises.

Notable Examples

Historical Events

The , one of the deadliest weather events in history, affected much of the Midwest and Northeast from late June through August, with temperatures exceeding 100°F (38°C) in many areas for weeks amid severe drought conditions. This prolonged episode resulted in approximately 5,000 deaths nationwide, primarily from heatstroke and related illnesses, overwhelming systems and infrastructure at the time. The event underscored the lethal potential of extreme heat in urban and rural settings, marking a pivotal moment in public awareness of heat-related risks during an era of limited meteorological tools. The 2003 European heat wave, spanning June to August, brought record-breaking temperatures across the continent, with experiencing daytime highs up to 40°C (104°F) for extended periods. It caused an estimated 70,000 excess deaths, disproportionately affecting older adults and those in urban areas due to poor and high . This catastrophe exposed gaps in preparedness, including inadequate early warning mechanisms, and directly spurred the development of heat-health warning systems throughout the . In the summer of 2010, western endured an unprecedented from late June to mid-August, with recording average temperatures 7–10°C above normal and peaks over 38°C (100°F). The event led to about 55,000 excess deaths, many in urban centers like where air quality deteriorated from widespread wildfires that burned over 500 sites and released massive smoke plumes. It highlighted urban vulnerabilities, such as heat-trapping concrete environments and strained emergency services, exacerbating mortality from cardiovascular and respiratory issues amid the smoke and heat. These historical events catalyzed key advancements in heat management. Following the heat waves, including , meteorological agencies improved forecasting capabilities through better observational networks, such as the introduction of radiosondes for upper-air data, enabling more reliable predictions of prolonged hot spells. The 2003 European crisis prompted policy reforms, notably France's establishment of the National Heatwave Plan (Plan National Canicule) in 2004, which integrated early warnings, public alerts, and healthcare coordination to mitigate future impacts. These responses emphasized proactive alerting and vulnerability reduction, shaping modern extreme heat warning frameworks.

Recent Incidents

In June 2021, the experienced a severe that brought temperatures exceeding 110°F (43°C) across parts of the and , marking an early precursor to formalized extreme heat warning systems. The event shattered numerous all-time records, with locations like , reaching 112°F (44°C) and Vancouver, British Columbia, hitting 111°F (44°C), prompting the (NWS) to issue widespread heat warnings emphasizing the life-threatening conditions. It resulted in over 600 deaths across the region, including more than 250 in the U.S. and 619 in alone, highlighting the dangers of prolonged extreme heat in typically temperate areas. The 2023 heat wave in the U.S. Southwest saw extreme heat warnings issued for , where sustained temperatures around 113°F (45°C) fueled record-breaking streaks of 110°F (43°C) or higher for 31 consecutive days. This event strained infrastructure, driving unprecedented energy demands as usage peaked, with Arizona's grid operator reporting all-time highs in consumption to meet cooling needs. NWS alerts urged residents to limit outdoor activities during peak heat, contributing to the year's total of 54 days above 110°F in . In late June 2025, a widespread affected much of the central and , impacting over 100 million people with record-setting temperatures and prompting extreme heat warnings across multiple states. Highs exceeded 100°F (38°C) in areas from the Midwest to the Northeast, with cities like and issuing alerts for heat indices over 105°F (41°C), leading to increased emergency visits and highlighting ongoing climate-driven risks. On May 13, 2025, the NWS issued an extreme heat warning for , , forecasting highs of 103°F to 106°F (39°C to 41°C) amid an early-season that broke monthly records. The advisory stressed , rest in cooled areas, and avoidance of strenuous activity, with actual highs reaching 103°F (39°C) initially and climbing to 106°F (41°C) by mid-week. No major fatalities were reported, thanks in part to proactive measures. Overall, extreme heat warnings have become more frequent since , with NOAA data indicating roughly twice as many heat events requiring alerts compared to earlier decades, driven by rising baseline temperatures.

Global Variations

International Standards

International standards for extreme heat warnings vary significantly across regions, reflecting differences in , , and vulnerabilities. In , particularly the , the Heat-Health Alert (HHA) system, operated jointly by the (UKHSA) and the , employs a tiered alerting framework based on forecasted maximum daytime and minimum nighttime temperatures. Alerts are issued from to , with thresholds tailored to regional climates: for , a alert triggers at daytime temperatures of 28.0–31.9°C or nighttime temperatures at or above the 95th of historical summer minima; alerts at 32.0–39.9°C daytime; and red alerts at 40.0°C or higher daytime. For other regions, thresholds are slightly lower, with at 27.0–29.9°C daytime, at 30.0–37.0°C, and red at 38.0°C or above. This impact-based system emphasizes coordination across sectors, with red alerts signaling risks to life for the general population and requiring responses. In , the Bureau of Meteorology's heatwave warning system categorizes events as low, severe, or extreme using the Excess Heat Factor (EHF), a metric that compares forecasted temperatures to the 95th of historical distributions for the location and time of year, integrated over at least three consecutive days. Warnings for severe or extreme heatwaves are issued up to four days in advance when temperatures exceed these percentiles across at least 10% of a weather district, highlighting heightened risks to health and infrastructure, including elevated bushfire danger through linkage with fire weather forecasts. This percentile-based approach accounts for local , ensuring relevance in diverse environments from urban centers to arid interiors. India's (IMD) issues heat wave warnings based on absolute temperature thresholds adjusted for regional norms, declaring a in plains regions when the maximum temperature reaches or exceeds 40°C, accompanied by a departure of at least 4.5°C from the long-term average; severe conditions apply above 47°C. In coastal areas, warnings are triggered when the maximum temperature reaches 37°C or more with a departure of at least 4.5°C from the normal maximum temperature, accounting for high humidity's role in exacerbating heat stress; these alerts often emphasize impacts on rural , such as crop wilting and losses. The system requires criteria to be met at two or more stations in a meteorological subdivision for at least two consecutive days. Key differences in these systems include variations in lead times and terminology, with developing nations like often providing shorter forecast horizons—typically 1–2 days—due to forecasting challenges, compared to 3–5 days in developed regions like the and . The (WHO) advocates for universal guidelines to standardize responses, recommending thresholds like a (WBGT) exceeding 35°C as a point beyond which sustained human activity becomes untenable without intervention, serving as a global benchmark for unlivable humid heat conditions despite national adaptations.

Climate Change Implications

Climate change, driven primarily by human activities such as greenhouse gas emissions, has unequivocally warmed the planet, with global surface temperatures having risen by approximately 1.2°C above pre-industrial levels (1850–1900) as of 2024. This warming has significantly increased the frequency and intensity of heatwaves, making extreme heat events more likely and severe than in a pre-industrial climate. According to the Intergovernmental Panel on Climate Change (IPCC), human influence has warmed the climate at an unprecedented rate, leading to more frequent compound extreme events, including heatwaves that now occur with higher probability due to elevated baseline temperatures. Projections indicate that these trends will intensify without substantial mitigation. , the number of heat days—defined as those exceeding the 99th of historical temperatures—could more than double or triple in many regions by 2050 under moderate emissions scenarios, according to analyses from the (NOAA). Globally, particularly in the , rising temperatures combined with humidity are pushing wet-bulb temperatures—the metric combining and moisture that determines —closer to critical thresholds. Studies project that under continued warming, parts of the humid could regularly approach or exceed 31–35°C wet-bulb temperatures, beyond which humans cannot effectively cool through sweating, posing lethal risks during prolonged exposure. The year 2024 exemplified this escalation, marking the warmest on record globally with temperatures exceeding 1.5°C above pre-industrial levels for the first time in a full , resulting in unprecedented stress across and increased issuance of heat warnings. Addressing these implications requires integrating extreme heat adaptation into international frameworks like the , which emphasizes limiting warming to well below 2°C while enhancing through Nationally Determined Contributions (NDCs). The Agreement's Global Goal on supports strategies to bolster heat vulnerability in vulnerable regions, potentially averting dozens of additional extreme hot days per year if emissions pathways align with 1.5–2°C targets. A key recommended measure is urban greening, such as expanding tree canopies and green roofs, which can mitigate effects by 0.5–2°C through shading and evaporative cooling, thereby reducing the need for heat warnings in densely populated areas. These adaptations, when scaled, could significantly offset the and economic burdens of escalating heat extremes.

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