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Air Quality in the Los Angeles Basin Increasingly Dependent on Temperature

Air Quality in the Los Angeles Basin Increasingly Dependent on Temperature

Research confirms that clean air and emission control policies have substantially reduced both PM 2.5 aerosol and ozone concentrations in the Los Angeles (LA) Basin over the last two decades. However, concentrations of both have plateaued in recent years. and high-pollutant events still regularly exceed accepted thresholds on hot days. The plateau and the role of heat are due to a shift in pollution sources, according to University of California, Berkeley researchers Clara Nussbaumer and Ronald C. Cohen. As pollutants from vehicle emissions decline, the response of pollutants from other sources to temperature is becoming an important factor in high-aerosol and high-ozone events in the megacity region. 

20 years of air quality data 

Nussbaumer and Cohen, funded in part by the NOAA Climate Program Office’s Atmospheric Chemistry, Carbon Cycle, & Climate (AC4) program, analyzed air quality data from across the LA Basin for the past two decades (1999-2018). The bulk of their data focuses on organic aerosols, a specific category of particulate matter with a diameter smaller than 2.5 micrometers (PM 2.5) linked to a range of respiratory and cardiovascular illness. They used data from 22 measurement sites across the LA Basin (eight in LA County, two in Orange County, five in Riverside County, four in San Bernardino County, and three in Ventura County) to study aerosols and four sites (three in LA, one in San Bernardino) to look at ozone. Their research was recently detailed in the scientific journal Environmental Science & Technology.

Based on measurements, concentrations of PM 2.5 in the LA Basin essentially halved from 1999 to 2012. After 2012, however, Nussbaumer and Cohen found that the PM 2.5 concentration at each site remained more or less constant. This sharp decline followed by a plateau suggests that while emission controls were targeting the largest sources of pollutants in 1999, such as vehicle emissions, as those sources were reduced over time the most prominent sources now are those unaffected by current emissions policies. 

While the average and max temperatures in the LA Basin have remained approximately constant over the last two decades, the relationship between temperature and aerosols has changed. Nussbaumer and Cohen’s analysis shows that when the temperature increases so too do PM 2.5 concentrations. Near the beginning of the 21st century, there was more variation in this relationship: if the temperature went up, sometimes PM 2.5 concentrations would increase a lot, sometimes a little. Now the relationship is more linear: if the temperature goes up, expect PM 2.5 concentrations to increase by a set amount for each degree rise in temperature.

As the relationship between aerosols and temperature becomes more clearly reflected in the observations it suggests that the decline in PM 2.5 is a result of a decrease in temperature-independent sources. Accordingly, from 2016-2018, there were nearly zero PM 2.5 violations at 68°F, while 70 to 80% of days over 100°F exceeded the National Ambient Air Quality Standard (NAAQS) threshold. “20 years ago, aerosol levels were unhealthy in LA no matter what the temperature,” Cohen explains, “but in the present it is only on the hotter days of the year.” 

Indirect sources play the primary role 

In 2018, organic aerosols comprised just under a quarter of PM 2.5 concentrations. Nussbaumer and Cohen found that organic aerosols were positively correlated with temperature and the largest contributor to high aerosol events.

Aerosol concentrations in LA have declined over time, leveling out around 2012. Credit: Nussbaumer and Cohen, Environ. Sci. Technol. 2021

Aerosols emitted directly into the atmosphere from combustion processes such as car exhaust, cooking, and wildfires are known as primary organic aerosol (POA). Secondary organic aerosol (SOA) form indirectly due to reactions of other emitted pollutants with sunlight. Nitrogen oxides (NOx) and volatile organic compounds (VOCs) are the usual precursors to any SOA; they also happen to be the same common prerequisites to ozone formation. 

Scientists have long recognized that SOA in rural locations are extremely temperature dependent. Nussbaumer and Cohen’s recent work shows this is now true in cities too. Their research seeks to illuminate what emission sources are responsible for these temperature-dependent SOA and what exactly their presence means for air quality control in the LA Basin and other megacity regions like LA. 

Targeting VOCs 

To determine SOA sources, Nussbaumer and Cohen first had to determine the role of various VOC precursors. They found that trends in VOC amounts in the air mirrored the trends in PM 2.5 concentrations. Early data records show multiple different sources of VOC molecules and that their emissions are less correlated with temperature. More recent records, however, show fewer sources with the majority of VOCs responding to temperature. 

Anthropogenic VOC emissions associated with vehicles in the LA Basin have steadily declined since 1999. They are now so low that the contribution of biogenic, or natural, VOC concentrations and chemicals from other sources such as emissions from household and industrial chemicals (collectively referred to as volatile chemical products or VCP) are now important players in the chemistry of ozone and SOA. Anthropogenic VOCs from industrial and motor vehicle emissions that form aerosol are closely related to the BTEX (benzene, toluene, ethylbenzene, and xylene) family of chemicals. The most common biogenic source of VOCs for LA Basin is isoprene, naturally emitted by plants such as the Mexican fan palm trees the region is famous for. 

Nussbaumer and Cohen created a back-of-the-envelope atmospheric model to test their conclusions about which chemical families are now running the aerosol show. They surmised that POA along with BTEX and isoprene together as SOA-precursors comprised the majority of the organic aerosols observed. Their model suggests that almost a quarter of the SOA in the LA Basin are formed by isoprene or other very similar compounds and these represent most of the temperature dependent increase. While there is evidence that some temperature-dependent VOCs have been controlled over time, such as those from evaporation of gasoline, isoprene is not one of them. 

“These results point to the exceptional success of control measures aimed at passenger vehicles,” Cohen notes, “and uncover new sources for high aerosol that are from other sectors. Possibly lawns and trees, but also possibly chemicals, solvents, and home cleaning products that evaporate more intensely when it is hot.”

The future of urban air quality 

Given the potential increase in temperature and heat wave intensity due to climate change, Nussbaumer and Cohen’s work indicates scientist and policy makers alike should pay attention to temperature-dependent aerosols. To keep an eye on California’s urban air quality, Cohen’s lab has maintained BEACO2N, a high-density network of measurements all over the Bay Area for years. All the collected data is publicly available for viewing and download. Many of the 75 locations with monitoring stations, are featured on the network's website. Cohen has also just started a collaboration with William Berelson at University of Southern California (USC) and the LA Unified School District to deploy BEACO2N nodes in LA. Separately, along with his UC Berkeley collaborator, Allen Goldstein, Cohen is partnering with NOAA scientists and the state and local air quality agencies on an experiment to observe emissions in LA at different temperatures. Combining these different observing strategies in the LA Basin, Cohen hopes, “will lead to better ideas for reducing high ozone and aerosol events in the Basin, ones that can then be used as a guide in other major cities suffering from poor air quality.” 

Read more about Nussbaumer and Cohen’s work on aerosols and ozone in Environmental Science & Technology »

More on the Cohen Atmospheric Chemistry Lab at Berkeley »

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HEAT FORECASTS

 

 

Current Temperature Probability Outlook

  • 6-10 Day
  • 8-14 Day
  • Month
  • Three Month Outlook
  • Weeks 3-4 Experimental Outlook Temperature Probability
 

6-10 Day Temperature Probability Outlook Map

 

6-10 Day Temperature Probability Outlook

In this map, shaded areas show where average temperature has an increased chance of being warmer or cooler than usual. The darker the shading, the greater the chance for the indicated condition. White areas have equal chances for average temperatures that are below, near, or above the long-term average for the month.

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8-14 Day Temperature Probability Outlook Map

 

8-14 Day Temperature Probability Outlook

In this map, shaded areas show where average temperature has an increased chance of being warmer or cooler than usual. The darker the shading, the greater the chance for the indicated condition. White areas have equal chances for average temperatures that are below, near, or above the long-term average for the month.

Learn More

 

One Month Temperature Probability Outlook

 

One Month Temperature Probability Outlook

In this map, shaded areas show where average temperature has an increased chance of being warmer or cooler than usual. The darker the shading, the greater the chance for the indicated condition. White areas have equal chances for average temperatures that are below, near, or above the long-term average for the month.

Learn More

 

Three Month Temperature Outlook

 

Three Month Temperature Outlook

In this map, shaded areas show where average temperature has an increased chance of being warmer or cooler than usual. The darker the shading, the greater the chance for the indicated condition. White areas have equal chances for average temperatures that are below, near, or above the long-term average for the month.

Learn More

 

Three Month Temperature Outlook

 

Weeks 3-4 Experimental Outlook Temperature Probability

In this experimental map, shaded areas show where average temperature has an increased chance of being warmer or cooler than usual. The darker the shading, the greater the chance for the indicated condition. White areas have equal chances for average temperatures that are below, near, or above the long-term average for the month.

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Current Heat Index Outlook

  • 8-14 Day Over 95°F
  • 8-14 Day Over 90°F for 2 Days
 

8-14 Day Over 95°F

 

8-14 Day Over 95°F

This map shows the probability that the Average Heat Index (which takes into consideration temperature and humidity) will exceed a given value over for at least 2 days in the forecast window.

 

8-14 Day Over 90°F for 2 Days

 

8-14 Day Over 90°F for 2 Days

This map shows the probability that the Average Heat Index (which takes into consideration temperature and humidity) will exceed a given value over for at least 2 days in the forecast window.

Global Tropical Hazards at Weeks 1 & 2

 

8-14 Day over 95°F

 

8-14 Day Over 95°F

This map shows global tropical hazards predicted by NOAA for the upcoming two week period. Orange and blue coloring indicates the level of confidence that above or below normal temperatures, respectively, will develop in the forecast window.

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UNDERSTANDING THE HEALTH RISK OF EXTREME HEAT

 

Health Outcomes

Exposure to extreme heat can have many direct effects on human health (heat stroke, reduced labor productivity), as well as indirect effects (promoting air pollution and increasing asthma attacks, overloading power grids requiring rolling blackouts). Negative health outcomes occur if an individual is exposed to the hazard and has not sufficiently adapted to reduce sensitivity.


Sensitivity

Sensitivity

Inherent characteristics of a person that make them vulnerable to heat, such as preexisting conditions, age, or occupation. To understand how to protect these groups, see Populations of Concern.

 

Adaptability

Adaptability

The ability of a person to take measures to reduce exposure and sensitivity - for example, avoiding outdoor activities during the day or wearing personal protective equipment (PPE) that is designed to mitigate heat buildup. When exposure is not preventable, adaptability can help reduce the impact of heat.

 

Exposure

Exposure

The extent to which an individual is exposed to extreme heat. Going outside on a hot, humid day and working in direct sunlight constitutes high exposure, while reducing exposure includes avoidance of these activities. Sometimes exposure is not preventable.

Climate conditions

Climate conditions

Climate conditions that create a heat hazard include direct sunlight, low winds, high humidity, and high temperatures. When these conditions exist, a heat hazard is created.

 

 

 

AT-RISK GROUPS

Higher summertime temperatures are linked to an increased risk of illnesses and death, particularly among certain groups. Select a group below to learn more.

 

Children

Read More

Emergency Responders

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Older Adults

Read More

Outdoor Workers

Read More

Athletes

Read More

Pets

Read More

 

 

 

 

 

HEAT WARNINGS IN YOUR AREA

View heat warnings in your area by state

 

 

 

STAYING SAFE DURING A HEAT WAVE

 

Key Safety Tips

  • Drink plenty of water; even if you do not feel thirsty. Avoid drinks with caffeine. Persons who have epilepsy or heart, kidney, or liver disease; are on fluid-restricted diets; or have a problem with fluid retention should consult a doctor before increasing liquid intake.
  • Never leave children or pets alone in closed vehicles.
  • Check on family, friends, and neighbors who do not have air conditioning and who spend much of their time alone.
  • Check on your animals frequently to ensure that they are not suffering from the heat.
  • Go to a designated public shelter if your home loses power during periods of extreme heat. Stay on the lowest floor out of the sunshine if air conditioning is not available.
  • Check the weather/listen to NOAA Weather Radio for critical updates from the National Weather Service (NWS).

 

 

Safety Tips If You Have To Go Outside

  • Avoid strenuous work during the warmest part of the day. Use a buddy system when working in extreme heat, and take frequent breaks.
  • Dress in loose-fitting, lightweight, and light-colored clothes that cover as much skin as possible. Avoid dark colors because they absorb the sun’s rays.
  • Protect face and head by wearing sunblock and a wide-brimmed hat.
  • Postpone outdoor games and activities.
  • Stay indoors as much as possible and limit exposure to the sun.

Additional Safety Tips

  • Eat well-balanced, light, and regular meals. Avoid using salt tablets unless directed to do so by a physician.
  • Limit intake of alcoholic beverages.
  • Avoid extreme temperature changes.
  • Consider spending the warmest part of the day in public buildings such as libraries, schools, movie theaters, shopping malls, and other community facilities. Circulating air can cool the body by increasing the perspiration rate of evaporation.
  • Download the FEMA App for heat advisories and safety tips.
  • Text SHELTER + your ZIP code to 43362 (4FEMA) to find the nearest shelter in your area (example: shelter 12345).

Safety Tips Before Extreme Heat Arrives

  • To begin preparing, you should build an emergency kit and make a family communications plan.
  • Know those in your neighborhood who are older, young, sick or overweight. They are more likely to become victims of excessive heat and may need help.
  • Be aware that people living in urban areas may be at greater risk from the effects of a prolonged heat wave than are people living in rural areas.
  • Get trained in first aid to learn how to treat heat-related emergencies.

Tips to Prepare Your Home

  • Install window air conditioners snugly; insulate if necessary.
  • Check air-conditioning ducts for proper insulation.
  • Install temporary window reflectors (for use between windows and drapes), such as aluminum foil-covered cardboard, to reflect heat back outside.
  • Weather-strip doors and sills to keep cool air in.
  • Cover windows that receive morning or afternoon sun with drapes, shades, awnings, or louvers. (Outdoor awnings or louvers can reduce the heat that enters a home by up to 80 percent.)
  • Keep storm windows up all year.

Heat Related Terms

Familiarize yourself with these terms to help identify an extreme heat hazard:

  • Heat Wave - Prolonged period of excessive heat, often combined with excessive humidity.
  • Heat Index - A number in degrees Fahrenheit (F) that tells how hot it feels when relative humidity is added to the air temperature. Exposure to full sunshine can increase the heat index by 15 degrees.
  • Heat Cramps - Muscular pains and spasms due to heavy exertion. Although heat cramps are the least severe, they are often the first signal that the body is having trouble with the heat.
  • Heat Exhaustion - Typically occurs when people exercise heavily or work in a hot, humid place where body fluids are lost through heavy sweating. Blood flow to the skin increases, causing blood flow to decrease to the vital organs. This results in a form of mild shock. If not treated, the victim's condition will worsen. Body temperature will keep rising and the victim may suffer heat stroke.
  • Heat Stroke - A life-threatening condition. The victim's temperature control system, which produces sweating to cool the body, stops working. The body temperature can rise so high that brain damage and death may result if the body is not cooled quickly.
  • Sun Stroke - Another term for heat stroke.
  • Excessive Heat Watch - Conditions are favorable for an excessive heat event to meet or exceed local Excessive Heat Warning criteria in the next 24 to 72 hours.
  • Excessive Heat Warning - Heat Index values are forecast to meet or exceed locally defined warning criteria for at least 2 days (daytime highs=105-110° Fahrenheit).
  • Heat Advisory - Heat Index values are forecast to meet locally defined advisory criteria for 1 to 2 days (daytime highs=100-105° Fahrenheit).

 

 


 

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NIHHIS is an integrated information system that builds understanding of the problem of extreme heat, defines demand for climate services that enhance societal resilience, develops science-based products and services from a sustained climate science research program, and improves capacity, communication, and societal understanding of the problem in order to reduce morbidity and mortality due to extreme heat.  NIHHIS is a jointly developed system by the Centers for Disease Control and Prevention (CDC) and the National Oceanic and Atmospheric Administration.

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