These data will help to guide the clinician in selecting the appropriate cervical orthosis for their adult patient based on comfort, morphologic considerations, and degree of immobilization required.
Non-malignant fibrosing tumors in the pediatric hand or juvenile fibromatoses are clinically challenging because of their relatively infrequent occurrence and because of the variety of names associated with these diseases. We conducted a review of a personal case series of pediatric patients with these tumors and discuss here the more common histologic types and clinical characteristics of the disease spectrum in the context of the available published literature. All histologic samples were reviewed by a single pathologist. Infantile myofibromatosis, fibrous hamartoma of infancy, juvenile aponeurotic fibromatosis, palmar fibromatosis (Dupuytren's type), infantile digital fibromatosis (Reye's tumor), fibroma of the tendon sheath, and melorheostosis represent the encountered lesions.
Abstract. Broadband snow albedo can range from 0.3 to 0.9 depending on microphysical
properties and light-absorbing particle (LAP) concentrations.
Beyond the widely observed direct and visibly apparent effect of darkening
snow, it is still unclear how LAPs influence snow albedo
feedbacks. To investigate LAPs' indirect effect on snow albedo feedbacks,
we developed and calibrated the Near-Infrared Emitting and Reflectance-Monitoring Dome
(NERD) and monitored bidirectional reflectance factors
(BRFs) hourly after depositing dust and black carbon (BC) particles onto experimental
snow surfaces.
After comparing snow infrared BRFs to snow specific surface areas (SSAs), we found that both measured and
modeled snow infrared BRFs are correlated with snow SSA.
These results, however, demonstrate a considerable uncertainty of ±10 m2 kg−1 in the determination of snow SSA from our BRF measurements.
The nondestructive technique for snow SSA retrieval that we present here
can be further developed for science applications that
require rapid in situ snow SSA measurements.
After adding large amounts of dust and BC to snow, we found more rapid decreasing of
snow BRFs and SSAs in snow with added LAPs compared to natural
(clean) snow but only during clear-sky conditions. These results suggest
that deposition of LAPs onto snow can accelerate snow
metamorphism via a net positive snow grain-size feedback.
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