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Evidence for an excess of B→D*τ(-)ν(τ) decays.
Based on the full BABAR data sample, we report improved measurements of the ratios R(D(*))=B(B[over ¯]→D(*)τ(-)ν[over ¯](τ))/B(B[over ¯]→D(*)ℓ(ℓ)(-)ν[over ¯](ℓ)), where ℓ is either e or μ. TheseExpand
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Remote Sensing Handbook for Tropical Coastal Management
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Mapping marine environments with IKONOS imagery: enhanced spatial resolution can deliver greater thematic accuracy
The IKONOS 2 satellite was launched in late 1999 and carries the first commercial multispectral instrument to achieve 4 m spatial resolution. The cost and accuracy of using IKONOS imagery to mapExpand
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The fishes of Saint Paul's Rocks
Fifty species of fishes are recorded from Saint Paul's Rocks in a checklist which includes notes on ecology and behaviour. The poor species diversity, which is the lowest of any tropical islandExpand
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Reef rehabilitation manual
This reef rehabilitation manual is intended to complement the reef restoration concepts and guidelines and provide more detailed hands-on advice, based on lessons-learnt from previous experience, onExpand
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Marine zoogeography of St Paul's Rocks
The zoogeographical relationships of the shallow water marine fauna of St Paul's Rocks (equatorial Atlantic) are examined with respect to ocean current patterns. Of seventy-seven benthic speciesExpand
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Searches for Lepton flavor violation in the decays tau{+/-}-->e{+/-}gamma and tau{+/-}-->mu{+/-}gamma.
Searches for lepton-flavor-violating decays of a tau lepton to a lighter mass lepton and a photon have been performed with the entire data set of (963+/-7)x10{6} tau decays collected by the BABARExpand
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Branching fraction and form-factor shape measurements of exclusive charmless semileptonic B decays, and determination of |V_{ub}|
We report the results of a study of the exclusive charmless semileptonic decays, B0→π-l+ν, B+→π0l+ν, B+→ωl+ν, B+→ηl+ν, and B+→η′l+ν (l=e or μ) undertaken with approximately 462×106 BB pairs collectedExpand
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Low-velocity zone atop the 410-km seismic discontinuity in the northwestern United States
The seismic discontinuity at 410 km depth in the Earth’s mantle is generally attributed to the phase transition of (Mg,Fe)2SiO4 (refs 1, 2) from the olivine to wadsleyite structure. Variation in theExpand
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