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Review article: The Foundation-Patuxent-Academy ice stream system, Antarctica

We review research about a group of fast-flowing Antarctic ice streams, the Foundation-Patuxent-Academy System. Previously, we knew little about how these ice streams flow, how they interact with each other and the ocean, what their geological history was, and how they might evolve in a warming world. By reviewing existing research, we have identified the future research needed to determine how these ice streams function, and how they might contribute to future global sea level rise.

Understanding changes in Iceland's streamflow dynamics in response to climate change

Iceland relies heavily on hydropower, making it important to understand changes in streamflow. Rivers reflect a warming, wetter climate, with rainfall increasingly replacing snowfall. Annual streamflow has generally increased, most notably during the cool season, while summer flows have declined in some non-glacial rivers. Glacial rivers show increasing melt-season flows over 1973–2023 but declining trends over 1993–2023, reflecting glacier retreat and recent North Atlantic sea surface cooling.

Detection and attribution of the role of anthropogenic climate change in industrial-era retreat of Pine Island Glacier

At least since we began measuring in detail, the West Antarctic Ice Sheet has lost a lot of ice, but we don't know precisely how important climate change is in this. Here, we put a number on the role of climate change in retreat of a glacier in this ice sheet, for the first time. We show that climate change made the shrinking of this glacier much worse. Our work also suggests that what happened on very long timescales (the last 10,000 years) might also matter for retreat of the ice sheets today.

Quantification of inmixing of Asian Monsoon air by multi-species classification in a match flight experiment

During the PHILEAS aircraft campaign a self-matching experiment was conducted to study the mixing of Asian Summer monsoon air into the upper troposphere – lower stratosphere. We present the first 3-D tomographic observations of this mixing for multiple trace gas species. We use advanced clustering to identify the types of air and their transport pathways, particularly into the stratosphere. Simulations of surface-origin tracers link several of these air types to different source regions.

Climate models with moderate climate sensitivity best simulate the magnitude of Earth's energy imbalance

Observations show an increasing imbalance between how much energy the Earth absorbs from the Sun and emits back to space, leading to climate change. We evaluate how well climate models simulate both the magnitude and trend of the imbalance. We find that models capture the magnitude but underestimate the trend, which is not related to how models handle volcanic aerosols when switching to future scenarios. The models that best simulate the magnitude are the ones with moderate climate sensitivity.

Air–Sea Interactions and Biogeochemical Responses to Medicane Daniel

This study examines Medicane Daniel, showing how a warm-core eddy (WCE), high ocean heat content (OHC), and a marine heatwave (MHW) sustained its intensity near Libya. Using high-resolution Surface Water and Ocean Topography (SWOT) observations, we reveal fine-scale eddy dynamics and larger WCE structures than those captured by conventional datasets, highlighting their role in air–sea interactions. Enhanced moisture convergence supported storm intensification, while storm-induced mixing and upwelling increased chlorophyll, nutrient, and oxygen concentrations.

Influence of tropospheric temperature on the formation and aging of secondary organic aerosol from biogenic vapor mixtures

We investigate how temperature (213–313K) affects secondary organic aerosol (SOA) particles derived from isoprene and α-pinene mixtures. Isoprene's suppression on α-pinene dimer formation varied with temperatures. Particles formed at higher temperatures are more oxidized yet more volatile than those formed at lower temperatures and then warmed. This work highlights the need to consider both temperature and biogenic vapor interaction to accurately describe SOA formation, aging, and global burden.

Estuarine mixing

This review presents major aspects of estuarine mixing. Due to the large amounts of brackish water in estuaries produced by mixing of fresh river discharge and salty ocean water, mixing is one major characteristic of what is an estuary. Mixing is quantified locally as well as on estuary-wide scales. Diagnostics of integrated mixing are given for estuarine volumes bounded by transects as well as surfaces of constant salinity moving with the flow. Examples for real-world estuaries are given.

Global and diurnal variations in tropospheric ammonia observed from a constellation of hyperspectral infrared sounders in three different LEO orbits

The diurnal cycle of NH₃ remains under-constrained at a global scale. To address this gap, we construct an integrated constellation with hyperspectral infrared sounders in three different Low-Earth-Orbits to achieve quasi-geostationary-like global monitoring coverage of NH₃ and provide six maps of global NH₃for every 4-hour in each day. This constellation has the potential to enhance the global climate-monitoring capacity of polar-orbiting meteorological satellites.

Chaotic fluctuations in Greenland ice streams limit predictability of ice sheet collapse

This model study sets out to investigate how the collapse of the Greenland ice sheet to a virtually ice-free state due to increasing temperatures depends on the rate of this increase. We find oscillations in ice volume on millennial timescales that impact the time it takes before the ice sheet collapses, concluding that there is a mode of deterministic chaos internal to the ice sheet dynamics.

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