Ice shelf collapse could trigger widespread retreat of marine‐based portions of the Antarctic ice sheet. However, little is known about the processes that control the stability of ice shelves. Recent observations have revealed that ice shelves have topographic features that span a spectrum of wavelengths, including basal channels and crevasses. Here we use ground‐penetrating radar data to quantify patterns of roughness within and between ice shelves. We find that roughness follows a power law with the scaling exponent approximately constant between ice shelves. However, the level of roughness varies by nearly an order of magnitude between ice shelves. Critically, we find that roughness strongly correlates with basal melt, suggesting that increased melt not only leads to larger melt channels, but also to increased fracturing, rifting and decreased ice shelf stability. This hints that the mechanical stability of ice shelves may be more tightly controlled by ocean forcing than previously thought.
It has long been recognized that vehicles emit more pollutants than allowed under the new car emission standards. Further tightening of the certification standards based on existing test procedures does not directly address the largest sources of emissions. This study attempts to quantify vehicle emissions by source, in order to prioritize future policymaking. Several new sets of data are used in conjunction with regulatory emission models to characterize the lifetime emissions from the average Model Year (MY)93 vehicle. Special attention is paid to two of the largest sources of real-world emissions: (1) high-power driving by cars with properly functioning emissions controls, and (2) cars with malfunctioning emissions controls. Emissions are projected to MY2000 and 2010, based on estimates of the effectiveness of recently adopted and proposed regulatory policies. These new policies are projected to reduce total emissions substantially.
Ice shelves have bumps in their topography that correspond to crevasses, melt channels and other features • We quantify the size of these bumps, called roughness, and find that the magnitude is spatially variable both between and within ice shelves • Roughness of different ice shelves strongly correlates with the magnitude of basal melt
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