D
David Long
Researcher at University College London
Publications - 338
Citations - 10139
David Long is an academic researcher from University College London. The author has contributed to research in topics: Coronal mass ejection & Solar flare. The author has an hindex of 49, co-authored 286 publications receiving 9270 citations. Previous affiliations of David Long include Wayne State University & Penn State Milton S. Hershey Medical Center.
Papers
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Journal ArticleDOI
An overview of perfluoroctylbromide--application as a synthetic oxygen carrier and imaging agent for X-ray, ultrasound and nuclear magnetic resonance.
David Long,D. Carl Long,Robert F. Mattrey,Raymond A. Long,Anthony R. Burgan,William C. Herrick,Dale F. Shellhamer +6 more
Journal ArticleDOI
Perfluoroctylbromide as a blood pool contrast agent for liver, spleen, and vascular imaging in computed tomography.
TL;DR: PFOB emulsion, in addition to hepatosplenic enhancement, produces prolonged and substantial opacification of the vascular space, allowing CT imaging of the heart and vascular structures minutes to hours after the end of infusion.
Patent
Method for extending the vascular dwell-time of particulate therapeutic and particulate diagnostic agents.
David Long,Raymond A. Long +1 more
TL;DR: In this article, a composition for increasing the vascular dwell-time of a particulate therapeutic or diagnostic agent in a mammal through the adjunct administration of an effective amount of the particulate medical or diagnostic agents and a vascular dwell time enhancing agent is presented.
Journal ArticleDOI
Understanding the Role of Mass-Unloading in Filament Eruptions
TL;DR: In this article, the authors describe a partial filament eruption on 11 December 2011 which demonstrates that the inclusion of mass is an important next step for understanding solar eruptions and demonstrate that flux cancellation and nearby flux emergence played a role in increasing the height of the filament prior to eruption.
Journal ArticleDOI
The English Channel ‘tsunami’ of 27 June 2011 : a probable meteorological source
TL;DR: In this article, a tsunami was caused by convective convective rainfallcells extending from the Bay of Biscay into the English Channel, and anomalous tides were experienced from Portugal to the Straits of Dover.