Waterlines: How Water Shapes Our World

jaywen
  • 5.0 (1)
  • Earth Sciences
  • Semiweekly

✦ Waterlines: How Water Shapes Our World ✦ explores the hidden role of water in shaping our planet, ecosystems, and daily lives. Each episode turns advanced water science into engaging, everyday conversations Designed for curious listeners — no scientific background required — the show features researchers, field stories, and real-world challenges that reveal why water matters more than we think. Whether you’re interested in the environment, climate, or how science connects to society, Waterlines helps you see the world through the lens of water.

  1. 2h ago

    Greenland’s Hidden Water: How Snow Aquifers May Open New Drains Through Ice

    Takeaway: On Helheim Glacier, hidden meltwater in the snow can turn small cracks into deep drains that let water reach the bed farther inland. Greenland’s ice sheet is not just melting at the edges. In some snowy high places, meltwater is stored inside the ice sheet like a buried, slushy reservoir—and where that hidden water finds cracks, it may change how glaciers move. This episode follows new work from Helheim Glacier in southeast Greenland, where researchers combine radar, satellite images, GPS stations, and fracture modeling to ask whether these underground firn aquifers can begin draining farther inland as the climate warms. We unpack what a firn aquifer is, why crevasses can become vertical pipes to the glacier bed, and why tiny changes in crack depth or water level may matter for ice flow, sea level, and the way scientists model Greenland’s future. The study is preliminary and careful: it identifies vulnerable places and early signs of change, not a finished forecast. Citation: Mejia JZ, Poinar K, Meyer CR, Sommers AN, Chu W (2025). Mechanisms for upstream migration of firn aquifer drainage: preliminary observations from Helheim Glacier, Greenland. Journal of Glaciology 71, e5, 1–11. https://doi.org/10.1017/jog.2024.78. This episode uses AI-generated voices.

    Greenland’s Hidden Water: How Snow Aquifers May Open New Drains Through Ice

  2. 2d ago

    Greenland’s Hidden Plumbing: Why Meltwater Timing Changes How Ice Slides

    Takeaway: On Greenland’s ice, meltwater can act like a delayed message: the farther it travels to reach a moulin, the later pressure builds below and the later the ice responds. Greenland’s summer melt is not just about how much water forms on the ice. It is also about timing: when that water reaches deep holes in the ice, when pressure builds underneath, and when the ice sheet starts to slide a little faster toward the sea. This episode follows field scientists working on the western Greenland Ice Sheet as they track daily pulses of meltwater from sunny surface streams, down vertical shafts called moulins, and into the dark drainage system beneath hundreds of meters of ice. The study shows that higher on the ice sheet, where moulins are fewer and surface catchments are larger, meltwater arrives later and pressure changes take longer to influence motion. That timing matters for understanding how Greenland responds to warming, how meltwater connects surface weather to ice movement, and why simple assumptions about ice-sheet plumbing can miss the rhythm of a real glacier. Citation: Mejia, J. Z., Gulley, J. D., Trunz, C., Covington, M. D., Bartholomaus, T. C., Breithaupt, C., et al. (2022). Moulin density controls the timing of peak pressurization within the Greenland Ice Sheet's subglacial drainage system. Geophysical Research Letters, 49, e2022GL100058. https://doi.org/10.1029/2022GL100058. Disclosure: this Waterlines episode package is written for public-science audio and uses AI-generated voices.

    Greenland’s Hidden Plumbing: Why Meltwater Timing Changes How Ice Slides

  3. 6d ago

    The Ice Sheet’s Hidden Drainpipes: Why Moulin Shape Changes Water Pressure Under Greenland

    Takeaway: Under Greenland’s ice, the shape of a moulin near its waterline can decide whether a day’s meltwater hits the glacier bed like a pulse or a cushion. Greenland’s summer meltwater does not simply run off the ice sheet like rain down a street. Much of it pours into deep vertical shafts called moulins, then rushes to the glacier bed, where water pressure can influence how ice slides toward the sea. This episode matters because the hidden plumbing under ice helps shape sea-level forecasts, field safety, and how scientists connect a warmer atmosphere to changes in glacier motion. We unpack a modeling study that asks a surprisingly concrete question: does the shape of a moulin matter? Many glacier models treat moulins like simple cylinders, but field explorers have found shafts that widen, pinch, curve, and open into chambers. Trunz and colleagues test idealized moulin shapes—cylinders, cones, hourglasses, diamonds, bottles, and goblets—to see how each one stores and releases meltwater. The key result is not that every twist in the ice matters equally. What matters most is the moulin’s size and shape near the range where the water level rises and falls each day. That “dynamic storage” can either amplify or dampen pulses of water pressure reaching the bed. Along the way, we explain moulins, subglacial channels, water pressure, why glacier beds can behave like wet brakes or slippery floors, and why better observations inside these icy shafts are still hard to get. We also talk through what this kind of simplified model can and cannot tell us about a real ice sheet full of connected drainage pathways. Paper featured: Trunz, C., Covington, M. D., Poinar, K., Andrews, L. C., Mejia, J., & Gulley, J. (2022). Modeling the influence of moulin shape on subglacial hydrology. Journal of Geophysical Research: Earth Surface, 127, e2022JF006674. https://doi.org/10.1029/2022JF006674 Disclosure: This Waterlines episode package is written for production with AI-generated host voices.

    The Ice Sheet’s Hidden Drainpipes: Why Moulin Shape Changes Water Pressure Under Greenland

  4. Oct 21

    Greenland’s Helheim Glacier: Why Ice Speed Depends on Both Ocean Edge and Hidden Water

    Takeaway: Helheim Glacier is steered by its ocean front near the coast, but farther inland the hidden water under the ice can take the wheel. Greenland’s outlet glaciers matter far beyond the Arctic because they help set the pace of sea-level rise, and that pace depends on something surprisingly everyday: where water goes. This episode follows new modeling work on Helheim Glacier, a fast-moving glacier that drains into the ocean in southeast Greenland. The study asks a deceptively simple question: when the glacier speeds up or slows down, is it mostly reacting to what happens at its ocean-facing front, or to meltwater slipping underneath the ice like water under a heavy sled? We unpack how the researchers coupled an ice-flow model with a subglacial water model to let ice motion and hidden drainage influence each other. Their result is not an either-or answer. Near the terminus, where the glacier meets the fjord, ocean-edge effects dominate speed changes for about 15 kilometers inland. Farther upstream, seasonal meltwater at the bed becomes the stronger control. In a warmer future with more melt reaching higher inland areas, that hidden plumbing could matter more for how much ice Greenland sends to the sea. Citation: Sommers, A. N., Meyer, C. R., Poinar, K., Mejia, J., Morlighem, M., Rajaram, H., Warburton, K. L. P., & Chu, W. (2024). Velocity of Greenland's Helheim Glacier controlled both by terminus effects and subglacial hydrology with distinct realms of influence. Geophysical Research Letters, 51, e2024GL109168. https://doi.org/10.1029/2024GL109168 Disclosure: This episode uses AI-generated voices.

    Greenland’s Helheim Glacier: Why Ice Speed Depends on Both Ocean Edge and Hidden Water

  5. Oct 16

    Greenland’s Ice Drains: How Giant Moulins Change the Pressure Under an Ice Sheet

    Takeaway: A moulin can act less like a drainpipe and more like a hidden water tank, softening daily pressure pulses under Greenland’s ice. Greenland’s meltwater does not just run across the surface and disappear. In summer, blue rivers plunge into holes in the ice and help decide how much water pressure builds at the bed of the ice sheet, where ice can slide faster toward the ocean. That matters for coastal communities, sea-level planning, and anyone trying to understand how a warming climate changes frozen landscapes from the inside out. In this episode of Waterlines, we explore a study that takes listeners into Greenland’s moulins: steep meltwater shafts that connect the surface of the ice sheet to its hidden drainage system below. Researchers measured water levels inside moulins, modeled how daily melt pulses move through the system, and directly explored two moulins with very different shapes. Their surprising finding: some moulins are far larger than many models have assumed, with storage spaces big enough to dampen daily pressure swings under the ice. We talk through what a moulin is, why subglacial water pressure matters for ice sliding, how a big hole can act like a water tank rather than a simple drainpipe, and why scientists still need many more observations before predicting how future melt will affect Greenland’s motion. We also discuss the field reality of studying these places: pressure sensors lowered into dark shafts, rope-access exploration, uncertainty in models, and the practical stakes for sea-level rise. Full paper citation: Covington, M. D., Gulley, J. D., Trunz, C., Mejia, J., & Gadd, W. (2020). Moulin volumes regulate subglacial water pressure on the Greenland Ice Sheet. Geophysical Research Letters, 47, e2020GL088901. https://doi.org/10.1029/2020GL088901 Disclosure: This episode uses AI-generated voices for the host conversation.

    Greenland’s Ice Drains: How Giant Moulins Change the Pressure Under an Ice Sheet

  6. Oct 14

    Greenland’s Cracks That Stay Put: What Crevasses Reveal About Meltwater and Ice Flow

    Takeaway: In Pâkitsoq, Greenland, the cracks mostly stayed put for ten years, but their changing size may shift where summer meltwater reaches the ice sheet’s hidden floor. Greenland’s ice sheet is not just melting at the edges; every summer, water also runs across its surface, finds openings, and may plunge toward the bed far below. That hidden plumbing matters because water at the base can change how fast ice slides toward the ocean. In this episode, we visit Pâkitsoq in central-western Greenland, where researchers used satellite radar and a new deep-learning tool called MimiNet to map crevasse fields year by year from 2015 to 2024. The surprising result: many crevasse fields stayed in the same places for a decade, while their total area grew and shrank from year to year with no clear long-term trend. We talk through what radar “sees,” why crevasses are different from moulins, how AI can help map ice-sheet hazards, and what the uncertainty means for understanding future sea-level rise. Citation: Khan N, Poinar K, Briner J, Nowicki S, Mejia JZ, Avellaneda A and Verné M (2026) Steady crevasse locations in Pâkitsoq, Greenland, over one decade: Results from MimiNet, a new deep-learning model for crevasse detection. Journal of Glaciology 72, e69, 1–19. https://doi.org/10.1017/jog.2026.10185 Disclosure: This Waterlines episode package is written for production using AI-generated voices.

    Greenland’s Cracks That Stay Put: What Crevasses Reveal About Meltwater and Ice Flow

  7. Oct 12

    When Greenland’s Meltwater Slows the Ice

    Takeaway: A sudden flood under Greenland’s ice can drain hidden water pockets at the bed, making the ice grip harder and slow down even while meltwater keeps flowing. Greenland’s summer melt does more than make rivers on the ice surface; it can change how the whole ice sheet grips the ground below. That matters because the speed of Greenland’s ice helps shape future sea level, coastal planning, and the way climate change shows up far from the Arctic. In this episode, we follow scientists to a moulin—a deep vertical drain in the ice—and listen as a hidden floodwave from draining surface lakes rushes under the ice sheet. The surprise: the flood did not simply carve bigger plumbing and speed things along. It appears to have drained hidden pockets of pressurized water at the bed, helping the ice stick more firmly and slow down to winter-like speeds. We unpack what moulins are, how researchers measure water pressure and ice motion in a dangerous, shifting landscape, and why Greenland may not behave like the smaller mountain glaciers scientists often use as examples. Citation: Mejia, J. Z., Gulley, J. D., Trunz, C., Covington, M. D., Bartholomaus, T. C., Xie, S., & Dixon, T. H. (2021). Isolated cavities dominate Greenland Ice Sheet dynamic response to lake drainage. Geophysical Research Letters, 48, e2021GL094762. https://doi.org/10.1029/2021GL094762. Disclosure: This Waterlines episode package is written for AI-generated host voices; the voices listeners hear are AI-generated.

    When Greenland’s Meltwater Slows the Ice

  8. Oct 9

    How Island Caves Breathe with the Tide

    Takeaway: On some limestone islands, caves that look cut off from the world can still pulse with the ocean through tiny connected holes in the rock. Coastal islands are not solid blocks of rock; many are more like old coral sand turned into Swiss cheese, with hidden pathways that can move seawater, freshwater, pollution, and even pressure from the ocean far inland. In this episode, we visit San Salvador Island in the Bahamas, where researchers used the rhythm of the tides to ask a deceptively simple question: are isolated coastal caves really isolated? The answer changes how we picture island aquifers, cave formation, and the underground plumbing that communities and ecosystems depend on. The study focuses on flank margin caves, rounded cave chambers that form inside young limestone near ancient freshwater lenses. Scientists long thought these caves mostly stored water but did not connect efficiently to larger flow networks until burial, cracking, or collapse. Breithaupt and colleagues tested that idea by measuring how ocean tides showed up in wells, boreholes, blue holes, and cave pools across rocks of different ages. Their results suggest older limestone can develop region-wide networks of connected solution pores, called touching vugs, and that some caves can plug into those networks before burial. Full paper citation: Breithaupt, C. I., Gulley, J. D., Moore, P. J., Fullmer, S. M., Kerans, C., & Mejia, J. Z. (2021). Flank margin caves can connect to regionally extensive touching vug networks before burial: Implications for cave formation and fluid flow. Earth Surface Processes and Landforms, 46, 1458–1481. https://doi.org/10.1002/esp.5114 Disclosure: This Waterlines episode package is written for public science listening and uses AI-generated host voices.

    How Island Caves Breathe with the Tide
See All (114)

About

✦ Waterlines: How Water Shapes Our World ✦ explores the hidden role of water in shaping our planet, ecosystems, and daily lives. Each episode turns advanced water science into engaging, everyday conversations Designed for curious listeners — no scientific background required — the show features researchers, field stories, and real-world challenges that reveal why water matters more than we think. Whether you’re interested in the environment, climate, or how science connects to society, Waterlines helps you see the world through the lens of water.

Information