An eddy-covariance flux tower near
irrigated cotton fields in San Joaquin Valley was installed in August 2023 at
the University of California Agriculture and Natural Resources experimental
fields to continuously measure exchanges of heat, moisture and momentum between
the land surface and atmosphere. Credit: Fan Wu
Outdoor air pollution is estimated
to contribute to more than 100,000 premature deaths in the United States each
year, according to the National Weather Service. Accurate air quality
forecasts—designed to protect public health, alerting communities to dangerous
levels of pollutants linked to asthma attacks, heart disease and premature
death—are critical for helping people limit exposure and for guiding regulatory
action.
However, a new study led by Fan Wu,
a doctoral student in Penn State's Department of Meteorology and Atmospheric
Science, suggests some of the computer models that agencies rely on may not be
getting it right. Wu and the multi-institutional team found that models used to
predict air pollution can seriously misrepresent how heat and moisture move
between farmland and the atmosphere, potentially skewing air quality forecasts
used for policy decisions.
The study, published in the journal Agricultural and Forest
Meteorology, evaluated how well the Weather Research and Forecasting (WRF)
model—a widely used regulatory weather model—simulates surface fluxes, which
are the exchanges of heat, moisture and momentum between the Earth's surface
and the atmosphere. These fluxes directly influence the atmospheric boundary
layer, the lowest part of the atmosphere that interacts with the surface and
contains the air people breathe. The depth and mixing of that layer are crucial
in determining how pollutants such as fine particles (PM 2.5) and ozone build
up or disperse.
The team evaluated the Pleim-Xiu
Land Surface Model (PX LSM), a land module within WRF used by air quality
agencies in California and the Mid-Atlantic region, including Pennsylvania and
Maryland. The researchers ran WRF simulations and compared the results to
yearlong, real-world measurements collected from 16 flux towers that directly
measure heat and moisture exchanges across California's San Joaquin Valley and
the Mid-Atlantic.
The team found that the model
performs very differently in the two regions.
Large errors over irrigated California fields
In California's San Joaquin Valley,
the model makes irrigated farm fields appear far too hot and dry. During summer
daylight hours, it overestimates the heat flowing from the surface to the
air—known as sensible heat flux—by about 260 watts per square meter, or 274%.
It also underestimates the cooling effect from evaporation—latent heat flux—by
about 200 watts per square meter, or 68%, especially during spring and summer
daylight hours. The problem stems from the model's exclusion of irrigation,
meaning it does not capture how added water cools and moistens the surface.
"These significant heat flux
errors over irrigated fields can distort air quality forecasts," Wu said.
"If the model puts too much heat into the atmosphere, it makes the
atmospheric boundary layer too deep, giving pollutants in the model more room
to dilute. That can lead to underestimates of pollution near the surface, where
people breathe."
Mid-Atlantic fares better but not perfectly
In the Mid-Atlantic, model errors
were smaller and more balanced. The system tended to slightly overestimate both
heating and evaporation, running too hot over cities and somewhat too wet over
vegetated areas. However, overall, it captured surface–atmosphere exchanges
more realistically than in California.
Across both regions, the
researchers also found that the model overestimates how strongly the surface
slows and stirs the wind during the daytime, with mixed performance at night.
The findings point to broader challenges in how the model represents surface–atmosphere
interactions. The researchers said the results also suggest that including a
representation of irrigation, perhaps by integrating space-based observations
of vegetation and soil moisture, could strengthen air quality forecasts in
heavily farmed regions.
Next steps to improve forecasting tools
"If WRF better represented
irrigation and land use details, we would expect more accurate simulations of
daytime PM2.5 and ozone concentrations in state modeling systems, which could
help agencies create more effective plans to reduce pollution," Wu said.
According to Ken Davis, professor
of meteorology and atmospheric science and research team member, the next step
is determining whether improving how models represent irrigation leads to
better air quality forecasts—and whether those improvements are practical for
states to adopt.
"We're testing whether tools
like NASA's Land Information System or a simpler irrigation module can reduce
the surface heat flux errors we identified," Davis said. "First, we
need to show that these approaches improve the weather model. Then we need to
determine whether states can realistically implement them. If they can,
adoption should be straightforward."
Davis added that the team must make
sure that improving the meteorology actually improves the air quality
simulation.
"Sometimes these complex systems contain compensating errors," Davis said. "If better surface modeling improves both the weather and air quality simulations—and early signs in the San Joaquin Valley suggest it does—then we're headed in the right direction."
Provided by Pennsylvania State University
Source: Irrigation gaps in weather models could skew air quality forecasts, study finds

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