Zobrazeno 1 - 10
of 57
pro vyhledávání: '"Carl G. Schmitt"'
Autor:
Christian Pilz, Michael Lonardi, Ulrike Egerer, Holger Siebert, André Ehrlich, Andrew J. Heymsfield, Carl G. Schmitt, Matthew D. Shupe, Birgit Wehner, Manfred Wendisch
Publikováno v:
Scientific Data, Vol 10, Iss 1, Pp 1-12 (2023)
Abstract During the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) expedition, the Balloon-bornE moduLar Utility for profilinG the lower Atmosphere (BELUGA) was deployed from an ice floe drifting in the Fram Strait fr
Externí odkaz:
https://doaj.org/article/25487e88a0074d618f3d77cb8cf9b29d
Publikováno v:
Atmosphere, Vol 13, Iss 5, p 824 (2022)
A new instrument for the quantification of light absorption by particles collected on filters has been developed to address long standing environmental questions about light-absorbing particles in air, water, and on snow and ice. The Light Absorption
Externí odkaz:
https://doaj.org/article/0650cb4b39e0461b9936130bb345eca6
Autor:
Carolina Soto Carrión, Carl G. Schmitt, Juan J. Zuñiga Negrón, Wilber Jiménez Mendoza, Oscar Arbieto Mamani, Rosmery S. Pozo Enciso, Sulema J. Guevara Sarmiento, Maxwell S. Rado Cuchills
Publikováno v:
Journal of Sustainable Development of Energy, Water and Environment Systems, Vol 9, Iss 1, Pp 0-0 (2021)
The presence of light-absorbing particles, including black carbon in glaciers leads to a reduction in albedo (light reflection), leading to further melting of snow ice, increased amount of shortwave solar radiation and leads to the glacier. The objec
Externí odkaz:
https://doaj.org/article/455dd078596445be832e3c64e0a7aa9b
Publikováno v:
Journal of the Atmospheric Sciences. 79:1651-1667
The Ice Particle and Aggregate Simulator (IPAS) is used to theoretically represent the aggregation process of ice crystals. Aggregates have a variety of formations based on initial ice particle size, shape, and falling orientation, all of which influ
Classification of Cloud Particle Imagery from Aircraft Platforms Using Convolutional Neural Networks
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 39:405-424
A vast amount of ice crystal imagery exists from a variety of field campaign initiatives that can be utilized for cloud microphysical research. Here, nine convolutional neural networks are used to classify particles into nine regimes on over 10 milli
Publikováno v:
Journal of the Atmospheric Sciences. 78:133-154
A novel methodology for modeling ice–ice aggregation is presented. This methodology combines a modified hydrodynamic collection algorithm with bulk aggregate characteristic information from an offline simulator that collects ice particles, namely,
Autor:
Michael Lonardi, Christian Pilz, Elisa F. Akansu, Sandro Dahlke, Ulrike Egerer, André Ehrlich, Hannes Griesche, Andrew J. Heymsfield, Benjamin Kirbus, Carl G. Schmitt, Matthew D. Shupe, Holger Siebert, Birgit Wehner, Manfred Wendisch
Publikováno v:
EPIC3Elementa: Science of the Anthropocene, 10(1), ISSN: 2325-1026
The tethered balloon-borne measurement system BELUGA (Balloon-bornE moduLar Utility for profilinG the lower Atmosphere) was deployed over the Arctic sea ice for 4 weeks in summer 2020 as part of the Multidisciplinary drifting Observatory for the Stud
Autor:
Zachary J. Lebo, Paul Connolly, Carl G. Schmitt, Vanessa Przybyo, Kara J. Sulia, Andrew J. Heymsfield
Publikováno v:
Journal of Applied Meteorology and Climatology. 58:1751-1761
The terminal velocity (Vt) of ice hydrometeors is of high importance to atmospheric modeling. Vt is governed by the physical characteristics of a hydrometeor, including mass and projected area, as well as environmental conditions. When liquid hydrome
Publikováno v:
Journal of the Atmospheric Sciences. 76:1903-1916
Testing the often-made assumption that ice particle aggregates (snowflakes) are well represented by oblate spheroids, ellipsoid fits are applied to aggregate images. An algorithm to retrieve both the ellipsoidal parameters and the orientations of the
Publikováno v:
Journal of the Atmospheric Sciences. 76:1661-1676
Aggregation, the process by which two or more ice particles attach to each other, is typically observed in clouds that span a range of temperatures and is influenced by the crystal shape (habit). In this study, the resulting characteristics of ice–