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1

Comparison of different methods to retrieve optical-equivalent snow grain size in central Antarctica

by T. Carlsen, G. Birnbaum, A. Ehrlich, J. Freitag, G. Heygster, L. Istomina, S. Kipfstuhl, A. Orsi, M. Schäfer, M. Wendisch
Published in The Cryosphere (2017)
“...The optical-equivalent snow grain size affects the reflectivity of snow surfaces and, thus...”

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2

A generalized photon-tracking approach to simulate spectral snow albedo and transmittance using X-ray microtomography and geometric optics

by T. Letcher, J. Parno, Z. Courville, L. Farnsworth, J. Olivier
Published in The Cryosphere (2022)
“...A majority of snow radiative transfer models (RTMs) treat snow as a collection of idealized grains...”

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3

Mapping liquid water content in snow at the millimeter scale: an intercomparison of mixed-phase optical property models using hyperspectral imaging and in situ measurements

by C. Donahue, S. M. Skiles, K. Hammonds
Published in The Cryosphere (2022)
“... model with varying LWC and grain size, and assessed against the in situ LWC sensor. Our results show...”

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4

Evaluation of E3SM land model snow simulations over the western United States

by D. Hao, G. Bisht, K. Rittger, T. Stillinger, E. Bair, Y. Gu, L. R. Leung
Published in The Cryosphere (2023)
“... complete (STC) snow-covered area and grain size (MODSCAG) and MODIS dust and radiative forcing in snow...”

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5

Comparison of a coupled snow thermodynamic and radiative transfer model with in situ active microwave signatures of snow-covered smooth first-year sea ice

by M. C. Fuller, T. Geldsetzer, J. Yackel, J. P. S. Gill
Published in The Cryosphere (2015)
“... against measured snow on sea-ice geophysical properties and against measured active microwave backscatter...”

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6

A composite 10 Be, IR-50 and 14 C chronology of the pre-Last Glacial Maximum (LGM) full ice extent of the western Patagonian Ice Sheet on the Isla de Chiloé, south Chile (42° S)

by J.-L. García, C. Lüthgens, R. M. Vega, Á. Rodés, A. S. Hein, S. A. Binnie
Published in E&G Quaternary Science Journal (2021)
“... profile, single grain infrared (IR) stimulated luminescence dating and 14 C samples to derive a new...”

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7

A probabilistic geologic model of the Krafla geothermal system constrained by gravimetric data

by Samuel W. Scott, Cari Covell, Egill Júlíusson, Águst Valfells, Juliet Newson, Birgir Hrafnkelsson, Halldór Pálsson, María Gudjónsdóttir
Published in Geothermal Energy (2019)
“... geophysical data allow 3D geologic models to be tested against measurements and geophysical anomalies...”

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8

Isotopic diffusion in ice enhanced by vein-water flow

by F. S. L. Ng
Published in The Cryosphere (2023)
“... “short-circuits” the slow diffusion within crystal grains to cause “excess diffusion”, enhancing the rate...”

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9

SNICAR-ADv3: a community tool for modeling spectral snow albedo

by M. G. Flanner, J. B. Arnheim, J. M. Cook, C. Dang, C. He, X. Huang, D. Singh, S. M. Skiles, C. A. Whicker, C. S. Zender
Published in Geoscientific Model Development (2021)
“... of constituent optical properties. The use of non-spherical ice grains, which scatter less strongly...”

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10

Creep and fracture of warm columnar freshwater ice

by I. E. Gharamti, J. P. Dempsey, A. Polojärvi, J. Tuhkuri
Published in The Cryosphere (2021)
“... about −0.3 ∘ C. The loading was applied in the direction normal to the columnar grains and consisted...”

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11

Formation mechanism of the Vaasa Batholith in the Fennoscandian shield: Petrographic and geochemical constraints

by H. Mäkitie, P. Sipilä, H. Kujala, A. Lindberg, A. Kotilainen
Published in Bulletin of the Geological Society of Finland (2012)
“...) with gradational contacts against the garnet- and cordierite-bearing diatexite and metatexite migmatites...”

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12

A new quantitative approach to identify reworking in Eocene to Miocene pollen records from offshore Antarctica using red fluorescence and digital imaging

by S. L. Strother, U. Salzmann, F. Sangiorgi, P. K. Bijl, J. Pross, C. Escutia, A. Salabarnada, M. J. Pound, J. Voss, J. Woodward
Published in Biogeosciences (2017)
“... sporomorph grains over longer non-successive geological timescales are easily identifiable within younger...”

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