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Keeping Humans in the Loop Improves Flood Forecasting

EOS - Tue, 05/19/2026 - 12:57
Source: Geophysical Research Letters  

Real-time hydrologic forecasting predicts river level and flooding inundation by combining continuously updated rainfall measurements, river gauge readings, and weather forecasts. Most of these flood forecasting systems depend on human interpretation and adjustments, or a “forecasters-in-the-loop” approach, which pairs computer models with a human expert on flood dynamics and local conditions. In contrast, in a “forecasters-over-the-loop” system, humans supervise automated forecasts and intervene only if necessary.

Recently, artificial intelligence (AI) and machine learning (ML) have become more integrated into flood prediction, and many of these systems are faster at processing large datasets and learning complex patterns from historical records than traditional models alone. But these new technologies also come with limitations—AI and ML require extensive data and may struggle to capture extreme, rare events.

Even though ML and AI are often touted as the future of flood forecasting, most studies have tested this technology against models that provide historical simulations, not the real-time operational systems that would be used during a flood. These simplified models may lack local details or are tested at daily rather than hourly resolution. Their effectiveness may be overestimated. 

Tran et al. produced the first study comparing the performance of ML models to an actual flood forecasting system used at the California Nevada River Forecast Center (CNRFC) that uses professional forecasters and traditional hydrologic models. The study suggests that a forecasters-in-the-loop approach outperforms the ML models in several key ways, including streamflow predictions and flood event detection, because forecasters can recognize model errors and account for poor input data—actions models cannot take on their own.

The researchers used data gathered from CNRFC river stage forecasts across 50 California and Nevada locations between 2012 and 2022 and river condition lead times from 1 to 96 hours. Compared to the ML models, the Community Hydrologic Prediction System used at CNRFC generally performed better at predicting stream flow and flood peaks, especially with longer lead times. Though the ML models could perform better at very short lead times, their accuracy declined quickly. Though automated forecasting options may seem promising, they are not yet a suitable replacement for human expertise when it comes to protecting lives and livelihoods from damaging floods, the researchers say. (Geophysical Research Letters, https://doi.org/10.1029/2025GL118317, 2026)

—Rebecca Owen (@beccapox.bsky.social), Science Writer

Citation: Owen. R. (2026), Keeping humans in the loop improves flood forecasting, Eos, 107, https://doi.org/10.1029/2026EO260161. Published on 19 May 2026. Text © 2026. AGU. CC BY-NC-ND 3.0
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Extreme weather events are accelerating tidal wetland loss, satellite data show

Phys.org: Earth science - Tue, 05/19/2026 - 09:00
Tidal wetlands are critical, yet vulnerable ecosystems. Tidal marshes, mangrove forests, and tidal flats support biodiversity, protect against flooding and storm surges, sequester carbon, and improve water quality. Due to human development and climate change, tidal wetland areas have been shrinking globally. A new study using 40 years of satellite data shows that this loss has been accelerating in the U.S. and that this acceleration is being increasingly driven by extreme weather events.

How much worse could western wildfires get? New modeling changes projections

Phys.org: Earth science - Tue, 05/19/2026 - 02:00
Across the western United States, wildfires are increasing in size and intensity. As the climate continues to warm, more extreme wildfires will reshape landscapes and pose a growing risk to human health and natural ecosystems throughout the West.

Seismicity and Stresses in the Eastern part of the Amazon Craton: Implications for the Intraplate Stress Field in South America

Geophysical Journal International - Tue, 05/19/2026 - 00:00
SummaryDespite generally low seismicity typical of intraplate regions, magnitudes larger than 6 have occurred in the Amazon craton. The installation of permanent stations of the Brazilian Seismic Network in the Amazon around 2014, the Vale 5-station network in the Carajás mineral province in 2019, and a 30-station temporary deployment (October2021-March/2024) significantly improved earthquake detectability in the eastern part of the Amazon craton. A review of the seismotectonic characteristics of the oldest, Eastern part of the Amazon craton is presented here. Seismicity is not uniform, and areas of higher seismicity are identified, such as in the northern part of the Tapajós-Parima province and along the eastern border of the craton. No clear correlation with the main trends of faults was observed. Contrary to Central and Eastern Brazil, seismicity is not directly correlated with lithospheric thin spots in the Amazon Craton but tends to occur in the flanks of thick keels (“craton edge” effect). A possible influence of free-air gravity anomalies was noticed suggesting that flexural stresses contribute to control seismicity. Five new focal mechanisms are presented for the eastern edge of the Amazon craton, indicating a stress field with NW-SE compression and NE-SW extension. An updated map of the stress field for mid-plate South America shows that the maximum horizontal stresses vary from E-W in SE Brazil, NW-SE in central Brazil and SW-NE in the north. This pattern can potentially be explained by upper mantle flow, provided more detailed convection models are used.

Rethinking Electrokinetic Signals Before Earthquakes: Insights from Finite-Fault Modeling

Geophysical Journal International - Tue, 05/19/2026 - 00:00
SummaryElectrokinetic signals generated by coupled stress–fluid processes are increasingly recognized as indicators of fault-zone dynamics prior to earthquakes. However, their interpretation is often limited by the common reliance on point-source approximations, which neglect the inherently distributed nature of stress accumulation and fluid migration along fault planes. Here, we develop a quasi-static finite-fault electrokinetic framework in which coupled stress and fluid perturbations are represented as spatially distributed, time-evolving sources. The approach combines an extended Luco–Apsel–Chen generalized reflection and transmission method with a point-source superposition scheme, enabling efficient simulation of electrokinetic responses to area sources in layered porous media. Numerical results reveal that the horizontal components of geoelectric fields in the coupled stress–fluid system are highly sensitive to fluid-source geometry, whereas vertical components primarily reflect stress loading. Spatial variability in initiation time, arising from finite-rate fluid migration, further introduces waveform complexity, amplitude modulation, and multi-stage temporal evolution in surface signals. Notably, we find that the directional variations of the geoelectric field provide a robust diagnostic for distinguishing fluid-driven from stress-induced signals, with angular misalignments reaching up to 16.6°. These results establish a quantitative framework for interpreting near-fault electrokinetic signals and for guiding monitoring strategies aimed at constraining fault-zone fluid pathways and stress evolution.

Sea level rise is swallowing US Mid-Atlantic farmland faster than expected, study finds

Phys.org: Earth science - Mon, 05/18/2026 - 22:10
Ghost forests, the cemetery-like groupings of dead trees killed by saltwater intrusion, have become haunting symbols of sea level rise overtaking land along the Mid-Atlantic coast. But a new study published in Nature Sustainability, led by William & Mary's Batten School & VIMS, points to even more dramatic land losses in the region's coastal farmlands, where the rate of marsh encroachment is happening nearly twice as fast.

Southern Ocean intermediate waters may hold key to Earth's carbon dioxide history

Phys.org: Earth science - Mon, 05/18/2026 - 20:00
Researchers at National Taiwan University and partner institutions have uncovered new evidence that Antarctic Intermediate Water (AAIW)—a distinct layer sitting 500–1,500 meters below the ocean surface—played a pivotal role in a major atmospheric carbon dioxide transition that occurred roughly 450,000 years ago.

Editorial Board

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s):

Multi-model evaluation and future projections of radio refractivity over West Africa using CMIP6

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Emmanuel Israel, Adeyemi Babatunde, Emmanuel G. Omolara

Integrating mechanism diagnosis and physics-guided machine learning for wind field simulation and speed correction in complex terrain

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Maorong Du, Jin Qian, Danni Chen, Zhongqi Liu, Chun Gao, Yi Lou

Mediterranean and global sea surface temperature trends to 2100: An ARIMAX time-series forecasting approach

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Alper Yildirim, Mehmet Bilgili, Arif Ozbek

Quantitative assessment of ionospheric F-region variability under different geomagnetic storm conditions during 24th and 25th solar cycle at a low-mid latitude station, New Delhi

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Ankit Gupta, Anshul Singh, Qadeer Ahmed, Aastha Rawat, Arti Bhardwaj, Puja Goel, A.K. Upadhayaya

A comparative assessment of machine learning and inhomogeneous Markov models for near-term aridity forecasting and trend analysis

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Abdol Rassoul Zarei

Estimating sporadic E horizontal drift parameters over central Europe: First results from Doppler sounding

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Habtamu Marew, Jaroslav Chum

Extreme scintillation structure diagnostics

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Charles Rino, Charles Carrano, Dmytro Vasylyev, Luca Spogli, Theodore Beach, Yu Morton, Keith Groves

Remote sensing of the ionosphere from very low earth orbit

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Timothy A. Cook, Supriya Chakrabarti

Integrating satellite-based atmospheric soundings and machine learning to correct radiosonde temperature biases

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Frederick M. Mashao, Danitza Klopper, Yehenew Kifle, Hector Chikoore, Ricardo K. Sakai, Kingsley K. Ayisi, Belay Demoz

Multiplatform observations and WRF-Based diagnosis of an extreme pre-monsoon convective outbreak over the Delhi National Capital Region, India

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Gargi Rakshit, Soumyajyoti Jana, Suryasnata Majumder, Jayanti Pal, Ashim Kumar Mitra, Ram Kumar Giri

A novel hybrid framework for wind speed prediction using decomposition and gated recurrent unit networks

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Gaurav Pandey, Rajneesh Sharma, Tushar Shikhola

Automated identification of Martian dust storms using AI-based approaches: A preparatory study for India's Mars Lander Mission (MLM)

Publication date: May 2026

Source: Journal of Atmospheric and Solar-Terrestrial Physics, Volume 282

Author(s): Bipasha Paul Shukla, Ankith B. Kumar, Mehul R. Pandya

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