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Atmospheric rivers (ARs) transport large amounts of moisture from the mid- to high-latitudes and they are a primary driver of the most extreme snowfall events, along with surface melting, in Antarctica. In this study, we characterize the climatology and surface impacts of ARs on West Antarctica, focusing on the Amundsen Sea Embayment and Marie Byrd Land. First, we develop a climatology of ARs in this region, using an Antarctic-specific AR detection tool combined with the Modern-Era Retrospective analysis for Research and Applications, version 2 (MERRA-2) and the European Centre for Medium-Range Weather Forecasts (ECMWF) Reanalysis v5 (ERA5) atmospheric reanalyses. We find that while ARs are infrequent (occurring 3 % of the time), they cause intense precipitation in short periods of time and account for 11 % of the annual surface accumulation. They are driven by the coupling of a blocking high over the Antarctic Peninsula with a low-pressure system known as the Amundsen Sea Low. Next, we use observations from automatic weather stations on Thwaites Eastern Ice Shelf with the firn model SNOWPACK and interferometric reflectometry (IR) to examine a case study of three ARs that made landfall in rapid succession from 2 to 8 February 2020, known as an AR family event. While accumulation dominates the surface impacts of the event on Thwaites Eastern Ice Shelf (> 100 kgm-2 or millimeters water equivalent), we find small amounts of surface melt as well (< 5 kgm-2). The results presented here enable us to quantify the past impacts of ARs on West Antarctica's surface mass balance (SMB) and characterize their interannual variability and trends, enabling a better assessment of future AR-driven changes in the SMB. [ABSTRACT FROM AUTHOR]

Atmospheric rivers (ARs) transport large amounts of moisture from the mid-to high-latitudes and they are a primary driver of the most extreme snowfall events on Antarctica. ARs also raise surface temperatures when they make landfall over Antarctica, leading to surface melting. In this study, we characterize the climatology and surface impacts of ARs on West Antarctica, focusing on the Amundsen Sea Embayment and Marie Byrd Land. First, we develop a climatology of ARs in this region, using an Antarctic-specific AR detection tool combined with MERRA-2 and ERA5 atmospheric reanalyses. We find that while ARs are infrequent, they cause intense precipitation in short periods of time and account for 11% of the annual surface accumulation. They are driven by the coupling of a blocking high over the Antarctic Peninsula with a low-pressure system known as the Amundsen Sea Low. Next, we use observations from automatic weather stations on Thwaites Eastern Ice Shelf to examine a case study of 3 ARs that made landfall in rapid succession from February 2 to 8, known as an AR family event. We use snow height observations to force the firn model SNOWPACK to reconstruct accumulation and surface melting during the event, and compare these results with accumulation higher up on the glacier derived from surface height changes using interferometric reflectometry. While accumulation dominates the surface impacts of the event on Thwaites Eastern Ice Shelf (>100 kg m-2), we find small amounts of surface melt as well (<5 kg m-2). West Antarctica currently experiences minimal surface melting, most of which is absorbed by the firn, but future atmospheric warming could lead to more widespread surface melting in West Antarctica. Combined with a future increase in AR intensity or frequency, this could limit the ability of the firn layer to absorb melt water, which could harm ice shelf stability, and ultimately accelerate mass loss of the West Antarctic Ice Sheet. The results presented here enable us to quantify the past impacts of ARs on West Antarctic surface mass balance and characterize their interannual variability and trends, enabling a better assessment of future AR-driven changes in the surface mass balance. [ABSTRACT FROM AUTHOR]

We evaluate several high-resolution remote sensing data products derived from WorldView-3 satellite imagery to determine which product or product grouping would be most applicable for identifying and mapping tropical tree species. The study site, La Selva Biological Station in Costa Rica, provides the infrastructure to facilitate collection of proper ground-truth data for image validation. An objective statistical analysis demonstrated that the WorldView-3 imagery, after applying a series of spectral and illumination image corrections, was able to accurately identify selected tree species. Specifically, this study defines the image bands and image-derived spectral vegetation indices that are the most effective for tree species discrimination. We show that corrected absolute reflectivity values from the green, red, red edge, and near-infrared are good differentiators of tropical tree species crowns. We also evaluate 14 possible multiband vegetation indices and show that two new indices developed here, using WorldView-3 image bands, have the highest discriminatory power for tropical tree species. A combination of both individual band information and vegetation indices would significantly improve image-based classification of tropical forests. [ABSTRACT FROM AUTHOR]

Examines the potential uses of multiangular remote sensing imagery for mapping and characterizing sea ice and ice sheet surfaces based on surface roughness properties. Concept of optical remote sensing; Specifications of spectral signature; Association of sea ice types with Multi-angle Imaging SpectroRadiometer.

Describes the broadscale geometry of the surface, bed, and internal layering of Simple Dome, Antarctica with focus on the near summit area, which is a potential site for deep coring. Global positioning system location of the surface at the summit; Results from radar profiling across the crest; Implication of the stratigraphy on the existence of Simple Dome.