Anika Raj All work
Fig. 01 · Machine-learning research · Illinois State Water Survey

Predicting Drought Across Illinois

Can weather and climate data from many sites forecast how drought hits soil, streams and vegetation?

Missing rain dries the soil first. If the shortfall lasts, it shows up later in rivers and in plants, and each of those stages is watched by a different monitoring system. Since summer 2026 I’ve been putting those systems on one scale to see how far ahead drought impacts can be forecast.

Role
Led the computational work: data pipelines, models, analysis and writing
Where
Illinois State Water Survey, Prairie Research Institute, University of Illinois Urbana-Champaign
Team
Mentor Dr. Allison Goodwell · co-author Kyla Wolski
Presenting
First-author abstract, 41st Conference on Hydrology, AMS Annual Meeting, Denver · January 14, 2027
01 · The network

Nineteen stations, one state

The Illinois Climate Network measures soil moisture and weather at 19 stations across the state, and some of its records go back to 1987. Each needle on the map is one station, reaching down into the soil it measures.

02 · Three systems, one scale

Drought moves from soil to streams and plants

Each stage is recorded by a different system: soil sensors at the stations, USGS stream gauges and Landsat satellite images. I built the pipelines that bring all three onto a common scale: more than 760,000 observations.

  • 602,868 stream-gauge records, 25 watersheds
  • 120,746 soil-moisture records, 19 stations
  • 36,971 satellite vegetation (NDVI) observations
03 · The bar to beat

Beat “tomorrow looks like today”

Soil moisture changes slowly, so repeating the latest reading is a hard forecast to beat. I made the test harder: the model never sees the most recent 14 days of soil readings, and the baseline repeats that two-week-old reading.

On held-out 2025 data, the model cut 5 cm soil-moisture error by 41.8%. Streamflow forecasts beat the same kind of baseline in all 25 watersheds, with a median error reduction of 27.7%.

04 · Depth

Near the surface, weather leads. Deeper down, memory does.

Share of day-to-day variation each source explained on its own:

At 5 cm
Weather
Old soil
44% vs 28%
At 50 cm
Weather
Old soil
6% vs 67%

“Old soil” is the two-week-old reading. From the August 2026 abstract.

05 · What weather missed

In 2023–24, the deep soil stayed dry

At 50 cm, soil moisture averaged 0.30 below its seasonal normal, but models fed only weather predicted about normal. Adding the two-week-old 50 cm reading shrank that miss from 0.32 to 0.10.

06 · One number, many places

A statewide score hides station differences

In an early test of 14-day forecasts, error at the hardest of 12 stations was 2.2× the easiest. That is why I report results station by station and by depth, not as one average.

07 · Beyond Illinois

Built to travel

The framework needs inputs that exist well beyond Illinois: weather and soil stations, stream gauges and satellite images. Where stations are sparse, reanalysis data such as ERA5-Land fills in every ~9 km grid cell, so I tested it against the station records and helped validate an ERA5-Land extraction pipeline at NCSA.

Why it matters

Interviews with 12 Illinois farmers pointed to the same need: soil-moisture information for where they farm.

Drought monitors describe conditions now. A forecast that says how soil, streams and plants will respond in the coming weeks gives people time to plan.

What comes next
  • 01Forecast impacts 14 days ahead using forecasted weather
  • 02Add streamflow, vegetation and more soil depths as forecast targets
  • 03Compare the results with the U.S. Drought Monitor
  • 04Test regional and station-specific models

The fine print

for the curious
How the forecasts work
  • Next-day soil-moisture forecasts with a 14-day observation delay, 12 lagged and weather predictors, and chronological train and test splits.
  • Linear, ridge, lasso and random-forest models, compared against delayed persistence. 2025 is held out for the final evaluation.
  • Random forest did best at 5 cm and linear regression at 50 cm, which integrates weather over longer periods.
How stations are paired with streams
  • Each station is linked to a stream gauge whose watershed contains it, not simply the nearest gauge: a station can sit near a gauge yet drain somewhere else.
  • Streamflow is a 14-day rolling mean, log-transformed and compared with each gauge’s seasonal normal.
Which numbers come from when
  • 41.8%, 25 of 25 watersheds, 27.7% and 760,000+ observations: the current results, evaluated on held-out 2025 data.
  • The depth comparison and the 2023–24 dry spell: the August 2026 abstract, evaluated before 2025.
  • Station-level error (Bondville and Brownstown): the July 2026 progress update, from an earlier 14-day forecasting setup.
About the map
  • Station positions are approximate: each sits at the place named in its Illinois State Water Survey station description.
  • Soil layers are not to scale. Rivers and lakes: Natural Earth.
  • The grid in the last view is drawn every 0.5°. ERA5-Land cells are about 0.1° (~9 km).
AMS Annual Meeting · Denver · January 14, 2027

Read the abstract

“Tracking Drought Propagation Across Soil Moisture, Streamflow, and Vegetation in Illinois Using Machine Learning,” 41st Conference on Hydrology. First author, with Kyla Wolski and Dr. Allison Goodwell.

Read the AMS abstract

Credits

with thanks
The team

Mentor and co-author

Mentor: Dr. Allison Goodwell, Illinois State Water Survey. Co-author: Kyla Wolski, Department of Civil and Environmental Engineering, University of Illinois Urbana-Champaign.

Feedback and collaboration

Shaped by expert critique

  • Dr. Savini Samarasinghe, on predictors and validation.
  • Dr. Trent Ford, Illinois State Climatologist, on separating soil-moisture forecasts from broader drought assessment.
  • Ben Galewski, National Center for Supercomputing Applications, on ERA5-Land data extraction.
Data

Public monitoring records

  • Illinois Climate Network, Illinois State Water Survey
  • USGS daily streamflow
  • Landsat vegetation index (NDVI)
  • ERA5-Land reanalysis