A glacial forebulge is a bending-related upheaval of the lithosphere that has a strong effect on the sea level change pattern and on lithospheric stresses, which can induce intraplate earthquakes.
Editors’ Vox
Posted inEditors' Vox
In Appreciation of AGU’s Outstanding Reviewers of 2024
AGU editors recognize the contributions of peer reviewers in 2024, whose expertise and dedication are integral to the advancement of the Earth and space sciences.
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Experienced Researcher Book Publishing: Sharing Deep Expertise
In the 3rd installment of career-focused articles, scientists who completed books as experienced researchers reflect on how their networks paved the way for—and grew during—the publishing process.
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Waterworks on Tree Stems: The Wonders of Stemflow
Stemflow hydrodynamics offers rich physics that seeks to describe water and matter cycling within the atmosphere-biosphere-geosphere with implications for water resources planning.
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Mid-Career Book Publishing: Bridging Experience with Discovery
In the 2nd installment of 3 career-focused articles, scientists contemplate why a book project was the perfect addition to the dynamic middle stage of their professional journeys.
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Early-Career Book Publishing: Growing Roots as Scholars
In the 1st installment of 3 career-focused articles, scientists who completed books as early-career researchers reflect on the positive outcomes the experience had on their professional development.
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Advances in Ecological Forecasting
AGU and ESA invite contributions to a cross-society special collection on ecological forecasting across ecosystems and scales.
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JGR: Space Physics Launches New Instrumentation Article Type
JGR: Space Physics welcomes new and original developments in instrumentation including novel experimental methodologies that are relevant to space physics.
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Groundwater Pollution in Karst Regions: Toward Better Models
New advances in modeling contaminant transport offer a clearer picture of how to protect karst aquifers.
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Water Tracks: The Veins of Thawing Landscapes
Tracing and tracking change in permafrost flowpaths could reveal the dynamics of warming poles.