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1. Regional flow conditions associated with stratocumulus cloud-eroding boundaries over the southeast Atlantic

   https://doi.org/10.1175/MWR-D-20-0250.1  

   Tomkins, Laura M.; Mechem, David B.; Yuter, Sandra E.; Rhodes, Spencer R. (March 2021, Monthly Weather Review)

   null (Ed.)

   Abstract Large, abrupt clearing events have been documented in the marine stratocumulus cloud deck over the subtropical Southeast Atlantic Ocean. In these events, clouds are rapidly eroded along a line hundreds–to–thousands of kilometers in length that generally moves westward away from the coast. Because marine stratocumulus clouds exert a strong cooling effect on the planet, any phenomenon that acts to erode large areas of low clouds may be climatically important. Previous satellite-based research suggests that the cloud-eroding boundaries may be caused by westward-propagating atmospheric gravity waves rather than simple advection of the cloud. The behavior of the coastal offshore flow, which is proposed as a fundamental physical mechanism associated with the clearing events, is explored using the Weather Research and Forecasting model. Results are presented from several week-long simulations in the month of May when cloud-eroding boundaries exhibit maximum frequency. Two simulations cover periods containing multiple cloud-eroding boundaries (active periods), and two other simulations cover periods without any cloud-eroding boundaries (null periods). Passive tracers and an analysis of mass flux are used to assess the character of the diurnal west-African coastal circulation. Results indicate that the active periods containing cloud-eroding boundaries regularly experience stronger and deeper nocturnal offshore flow from the continent above the marine boundary layer, compared to the null periods. Additionally, we find that the boundary layer height is higher in the null periods than in the active periods, suggesting that the active periods are associated with areas of thinner clouds that may be more susceptible to cloud erosion. 

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2. Take the Long Way Home—Distant Peering to the Cloud

   https://doi.org/10.1109/TON.2025.3598634  

   Carisimo, Esteban; Weaver, Mia; Bustamante, Fabián E; Barford, Paul (January 2026, IEEE Transactions on Networking)

   The emergence of large cloud providers in the last decade has transformed the Internet, resulting in a seemingly ever-growing set of datacenters, points of presence, and network peers. Despite the availability of closer peering locations, some networks continue to peer with cloud providers at distant locations, traveling thousands of kilometers. In this paper, we employ a novel cloud-based traceroute campaign to characterize the distances networks travel to peer with the cloud. This unique approach allows us to gain unprecedented insights into the peering patterns of networks. Our findings reveal that 50% of the networks peer within 300 kilometers of the nearest datacenter. However, our analysis also reveals that over 20% of networks travel at least 6,700 kilometers beyond the proximity of the nearest computing facility, and some as much as 18,791 kilometers! While these networks connect with the cloud worldwide, from South America to Europe and Asia, many come to peer with cloud providers in North America, even from Oceania and Asia. We explore possible motivations for the persistence of distant peering, discussing factors such as cost-effective routes, enhanced peering opportunities, and access to exclusive content. 

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3. Waterfalls Alter Reach‐Scale Fluvial Erosion Rates: Evidence From Field Data and Process Modeling

   https://doi.org/10.1029/2024JF007792  

   Rothman, Sophie D; Scheingross, Joel S; McCoy, Scott W (December 2024, Journal of Geophysical Research: Earth Surface)

   Waterfalls are often interpreted as transient, upstream‐propagating features that mark changes in external conditions. Thus, waterfalls are commonly used to infer past tectonic and climatic forcing, making understanding the controls on waterfall erosion central to predicting how external perturbations move through landscapes. Surprisingly, there exist few direct field measurements of waterfall erosion, and existing waterfall retreat measurements are rarely paired with measurements of waterfall morphology and frequency, which, theory suggests, modulate retreat rates. This lack of data limits our ability to test existing theory and explore how waterfalls alter reach‐scale bedrock erosion rates. Here, we use cosmogenic¹⁰Be accumulated in bedrock riverbeds to measure erosion rates in fluvial reaches with varying waterfall frequency and morphology. We find that waterfall‐rich reaches erode one to five times faster than the landscape average, and that reach‐averaged erosion rates increase with increasing waterfall frequency. We develop a new, process‐based model combining waterfall and planar‐channel erosion to explore mechanistic controls on the relative erosion rate between waterfall‐rich and waterfall‐free reaches. This model predicts that reach‐averaged erosion rates increase with waterfall frequency at low sediment supply, consistent with our field measurements, but that waterfalls can also slow reach‐averaged erosion rates for high sediment supply, large grain sizes, low water discharge, or large plunge pools. Our work is consistent with previous suggestions that waterfall erosion rates may decrease in low drainage areas and can influence long‐profile morphology. 

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4. Large-scale state and evolution of the atmosphere and ocean during PISTON 2018

   https://doi.org/10.1175/JCLI-D-20-0517.1  

   Sobel, Adam H.; Sprintall, Janet; Maloney, Eric D.; Martin, Zane K.; Wang, Shuguang; de Szoeke, Simon P.; Trabing, Benjamin C.; Rutledge, Steven A. (March 2021, Journal of Climate)

   null (Ed.)

   Abstract The Propagation of Intraseasonal Tropical Oscillations (PISTON) experiment conducted a field campaign inAugust-October 2018. The R/V Thomas G. Thompson made two cruises in thewestern North Pacific region north of Palau and east of the Philippines. Using select field observations and global observational and reanalysis data sets, this study describes the large-scale state and evolution of the atmosphere and ocean during these cruises. Intraseasonal variability was weak during the field program, except for a period of suppressed convection in October. Tropical cyclone activity, on the other hand, was strong. Variability at the ship location was characterized by periods of low-level easterly atmospheric flow with embedded westward propagating synoptic-scale atmospheric disturbances, punctuated by periods of strong low-level westerly winds that were both connected to the Asian monsoon westerlies and associated with tropical cyclones. In the most dramatic case, westerlies persisted for days during and after tropical cyclone Jebi had passed to the north of the ship. In these periods, the sea surface temperature was reduced by a couple of degrees by both wind mixing and net surface heat fluxes that were strongly (~200 Wm −2 ) out of the ocean, due to both large latent heat flux and cloud shading associated with widespread deep convection. Underway conductivity-temperature transects showed dramatic cooling and deepening of the ocean mixed layer and erosion of the barrier layer after the passage of Typhoon Mangkhut due to entrainment of cooler water from below. Strong zonal currents observed over at least the upper 400 meters were likely related to the generation and propagation of near-inertial currents. 

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5. Mesoscale Ionospheric Structures and Very Large Geomagnetic Disturbances at High Latitudes

   https://doi.org/10.1029/2025JA033818  

   Engebretson, Mark J; Weygand, James M; Nishimura, Yukitoshi; Moldwin, Mark B; Steinmetz, Erik S; Ochoa, Jesus A; Pilipenko, Vyacheslav A; Gjerloev, Jesper (August 2025, Journal of Geophysical Research: Space Physics)

   Abstract Auroral substorms that move from auroral (<70°) to polar (>70°) magnetic latitudes (MLAT) are known to occur preferentially when a high‐speed solar wind stream passes by Earth. We report here on observations that occurred during a ∼75‐min interval with high‐speed solar wind on 28 November 2022 during which auroral arcs and very large geomagnetic disturbances (GMDs), also known as magnetic perturbation events (MPEs), with amplitude >9 nT/s = 540 nT/min moved progressively poleward at eight stations spanning a large region near and north of Hudson Bay, Canada shortly before midnight local time. Sustained GMD activity with amplitudes >3 nT/s appeared at each station for durations from 13 to 25 min. Spherical Elementary Currents Systems maps showed the poleward movement of a large‐scale westward electrojet as well as mesoscale electrojet structures and highly localized up/down pairs of vertical currents near these stations when the largest GMDs were observed. This study is consistent with other recent studies showing that very large poleward‐progressing GMDs can occur under high Vsw conditions, but is the first to document the sustained occurrence of large GMDs over such a wide high‐latitude region. 

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