Laurence C. Smith
· John Atwater and Diana Nelson University Professor of Environment and Society, Professor of Earth, Environmental and Planetary SciencesVerifiedBrown University · Environmental Studies
Active 1939–2025
About
Laurence C. Smith is a member of the Northern Change Research team at Brown University, which has a long history of excellence in Arctic studies and polar research. The research activities associated with Brown's Arctic@Brown initiative suggest a focus on environmental and geographic changes in Arctic regions, including sea ice travel conditions, river dynamics, and resource development in Greenland. As part of the Institute at Brown for Environment and Society (IBES), Smith contributes to understanding environmental processes and societal impacts in polar environments, leveraging remote sensing, modeling, and field data to address pressing ecological and geopolitical questions related to the Arctic.
Research topics
- Climatology
- Geology
- Oceanography
- Physical geography
- Environmental science
- Geography
- Ecology
- Biology
- Geomorphology
Selected publications
UNC Libraries · 2025-08-02
articleOpen accessLobe-Switching Avulsions: Delta Geometry Could Determine Locations
Research Square · 2025-09-25
preprintOpen accessSenior authorEuclid Quick Data Release (Q1): VIS processing and data products
ArXiv.org · 2025-03-19
preprintOpen accessThis paper describes the VIS Processing Function (VIS PF) of the Euclid ground segment pipeline, which processes and calibrates raw data from the VIS camera. We present the algorithms used in each processing element, along with a description of the on-orbit performance of VIS PF, based on Performance Verification (PV) and Q1 data. We demonstrate that the principal performance metrics (image quality, astrometric accuracy, photometric calibration) are within pre-launch specifications. The image-to-image photometric scatter is less than $0.8\%$, and absolute astrometric accuracy compared to Gaia is $5$ mas Image quality is stable over all Q1 images with a full width at half maximum (FWHM) of $0.\!^{\prime\prime}16$. The stacked images (combining four nominal and two short exposures) reach $I_\mathrm{E} = 25.6$ ($10σ$, measured as the variance of $1.\!^{\prime\prime}3$ diameter apertures). We also describe quality control metrics provided with each image, and an appendix provides a detailed description of the provided data products. The excellent quality of these images demonstrates the immense potential of Euclid VIS data for weak lensing. VIS data, covering most of the extragalactic sky, will provide a lasting high-resolution atlas of the Universe.
2025-02-07
preprintOpen accessAbstract. Increasing outburst flood hazards from melting glaciers threaten Himalayan communities but are difficult to assess. On 16 August 2024, a catastrophic Glacial Lake Outburst Flood (GLOF) occurred unexpectedly in the Bhotekoshi River Valley, in the Mt. Everest region of Nepal. Using this disaster as an illustration, we demonstrate that combining new and legacy satellite remote sensing technologies for lake water level, turbidity, and extent can detect potential GLOF hazards and help identify these risks.
2025-09-29
articleOpen accessThe Surface Water and Ocean Topography (SWOT, launched in December 2022) satellite has the potential to improve knowledge of river discharge globally, but preliminary SWOT discharge estimates are prone to timeseries bias, mainly induced by globally available prior information. To address this issue, we present a new algorithm designed to improve SWOT discharge. SFOI analytically integrates basin-scale information by applying mass conservation to time averaged SWOT discharge and estimates of regionalized runoff. We test the algorithm on three river basins with drainage areas on the order of 105 km2. We find that when the time averaged SWOT discharge observations are spatially unbiased (i.e. their spatially averaged error is close to zero) the algorithm significantly improves SWOT discharge: the median (interquartile range) absolute value of the normalized SFOI error is 15% (10-19%) for the Willamette River basin, and 12% (7-48%) for the upper Ohio River basin, significant improvements over SWOT discharge error (median values of 30% and 31%, respectively). However, for the Loire River basin, which has high (~60%) spatial bias, the algorithm does not improve SWOT discharge. These results imply that understanding and reducing spatial bias at the basin scale is key for reducing temporal bias in river discharge timeseries. Assessing spatial bias globally, we find that SWOT discharge should achieve its target accuracy (30% discharge error, with most of it temporal bias) even in ungaged basins, enabling SWOT discharge to provide significant improvements to the global water budget.
A First Look at River Discharge Estimation From SWOT Satellite Observations
Geophysical Research Letters · 2025-05-03 · 36 citations
articleOpen accessAbstract The Surface Water and Ocean Topography (SWOT) satellite has the potential to transform global hydrologic science by offering simultaneous and synoptic estimates of river discharge and other hydraulic variables. Discharge is estimated from SWOT observations of water surface elevation, width, and slope. A first assessment using just the highest quality SWOT measurements, over the first 15 months (March 2023–July 2024) of the mission evaluated at 65 gauged reaches shows results consistent with pre‐launch expectations. SWOT estimates track discharge dynamics without relying on any gauge information: median correlation is 0.73, with a correlation interquartile range of 0.51–0.89. SWOT estimates capture discharge magnitude correctly in some cases but are biased (median bias is 50%) in others. There are already a total of 11,274 ungauged global locations with highest quality SWOT measurements where SWOT discharge is expected to accurately track discharge variations: this value will increase as SWOT data record length grows, algorithms are refined and SWOT measurements are reprocessed. This first look indicates that SWOT discharge is performing as expected for SWOT data that achieve performance requirements, providing observed information on discharge variations in ungauged basins globally.
Euclid Quick Data Release (Q1). VIS processing and data products
Astronomy and Astrophysics · 2025-07-22 · 2 citations
articleOpen accessThis paper describes the VIS PF of the Euclid ground segment pipeline, which processes and calibrates raw data from the VIS camera. We present the algorithms used in each processing element along with a description of the on-orbit performance of VIS PF based on performance verification and Q1 datasets. We demonstrate that the principal performance metrics (image quality, astrometric accuracy, photometric calibration) are within pre-launch specifications. The image-to-image photometric scatter is less than percent and absolute astrometric accuracy compared to Gaia is 5,mas. Image quality is stable over all Q1 images, with a FWHM of . The stacked images (combining four nominal and two short exposures) reach IE=25.6 ($10,σ$, measured as the variance of diameter apertures). We also describe quality control metrics provided with each image, and an appendix provides a detailed description of the provided data products. The excellent quality of these images demonstrates the immense potential of Euclid VIS data for weak lensing. VIS data covering most of the extragalactic sky will provide a lasting high-resolution atlas of the Universe.
2025-02-07 · 1 citations
preprint2025-06-20
preprintOpen accessThe preprint version of this work has now been formally published. Going forward, please cite the final WRR publication instead of the preprint : Wang, J., Pottier, C., Cazals, C., Battude, M., Sheng, Y., Song, C., Sikder, M.S., Yang, X., Ke, L., Delhoume, M., Gosset, M., Oliveira, R.R.A., Grippa, M., Girard, F., Allen, G.H., Xu, X., Zhu, X., Biancamaria, S., Smith, L.C., Crétaux, J.-F., and Pavelsky, T. (2025). The Surface Water and Ocean Topography Mission (SWOT) Prior Lake Database (PLD): Lake mask and operational auxiliaries. Water Resources Research , 61, e2023WR036896. https://doi.org/10.1029/2023WR036896
Greenland ice sheet runoff reduced by meltwater refreezing in bare ice
Nature Communications · 2025-09-12 · 1 citations
articleOpen accessAbstract The contribution of Greenland Ice Sheet meltwater runoff to global sea-level rise is accelerating due to increased melting of its bare-ice ablation zone. There is growing evidence, however, that climate models overestimate runoff from this critical area of the ice sheet. Climate models traditionally assume that all bare-ice runoff enters the ocean, unlike porous firn, in which some meltwater is retained and/or refrozen. We used field measurements and numerical modeling to reveal that extensive retention and refreezing also occurs in bare glacier ice. We found that, from 2009 to 2018, meltwater refreezing in bare, porous glacier ice reduced runoff by an estimated 11–17 Gt a −1 in southwest Greenland alone, equivalent to 9–15% of this sector’s annual meltwater runoff simulated by climate models. This mass retention explains evidence from prior studies of runoff overestimation on bare ice by current generation climate models and may represent an overlooked buffer on projected runoff increases. Inclusion of bare-ice retention and refreezing processes in climate models therefore has immediate potential to improve forecasts of ice sheet runoff and its contribution to sea-level rise.
Recent grants
Sensitivity of the West Siberian Lowland to Past and Present Climate
NSF · $752k · 1999–2002
Frequent coauthors
- 188 shared
L. H. Pitcher
Oak Ridge Institute for Science and Education
- 107 shared
Sarah Cooley
- 101 shared
Jonathan C. Ryan
- 100 shared
Ethan D. Kyzivat
Brown University
- 98 shared
Å. K. Rennermalm
Rutgers, The State University of New Jersey
- 91 shared
Tamlin M. Pavelsky
- 90 shared
C. J. Gleason
University of Massachusetts Amherst
- 78 shared
M. G. Cooper
Pacific Northwest National Laboratory
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