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The top documents tagged [earth tides]

Earth-Moon System Section 25.2. Earth’s Moon The moon is about 384,000 kilometers away from the Earth Moon’s gravity is too weak to hold onto gas molecules,
Earth-Moon System Section 25.2. Earth’s Moon The moon is about 384,000 kilometers away from the Earth Moon’s gravity is too weak to hold onto gas molecules,
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Stable levelling and locking methods applicable for borehole very broad band seismic sensors including tilt meters presented at SUPERSITES COORDINATION
Stable levelling and locking methods applicable for borehole very broad band seismic sensors including tilt meters presented at SUPERSITES COORDINATION
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Lecture-19 1 Lecture #19- Seismometers. Lecture-19 2 Seismic Instrumentation F Devising systems that can accurately measure and record ground motions
Lecture-19 1 Lecture #19- Seismometers. Lecture-19 2 Seismic Instrumentation F Devising systems that can accurately measure and record ground motions
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Performance of the LIGO Pre-stabilized Laser System Rick Savage LIGO Hanford Observatory Ninth Marcel Grossmann Meeting on General Relativity Rome 2000
Performance of the LIGO Pre-stabilized Laser System Rick Savage LIGO Hanford Observatory Ninth Marcel Grossmann Meeting on General Relativity Rome 2000
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LIGO-G020486-00-W Commissioning Data on Vibration Isolation & Suspensions Fred Raab 24 October 02
LIGO-G020486-00-W Commissioning Data on Vibration Isolation & Suspensions Fred Raab 24 October 02
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GRAVITY. EARTH’S GRAVITY FIELD 978 Gals 983 Gals 1 Gal = 1 cm/sec² ELLIPSOID North-South change ~1 mGals/km ~1.5 mGals/mile ~1 Gals/m ~.3 Gals/ft
GRAVITY. EARTH’S GRAVITY FIELD 978 Gals 983 Gals 1 Gal = 1 cm/sec² ELLIPSOID North-South change ~1 mGals/km ~1.5 mGals/mile ~1 Gals/m ~.3 Gals/ft
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Currents. Driven by forces of wind, tides, and gravity, currents keep the ocean in constant motion. 7 Major Currents West Wind Drift (AKA=Antarctic Circumpolar
Currents. Driven by forces of wind, tides, and gravity, currents keep the ocean in constant motion. 7 Major Currents West Wind Drift (AKA=Antarctic Circumpolar
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The Earth is not a sphere: The horizontal component of geodesy Dr. Dru Smith Chief Geodesist, National Geodetic Survey National Science Teacher’s Association
The Earth is not a sphere: The horizontal component of geodesy Dr. Dru Smith Chief Geodesist, National Geodetic Survey National Science Teacher’s Association
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Ph.D student at LMV/Chalmers
Ph.D student at LMV/Chalmers
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GPS Services Group C&C Technologies, Inc., C-Nav GcGPS System Background and Accuracy
GPS Services Group C&C Technologies, Inc., C-Nav GcGPS System Background and Accuracy
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Wiesław Kosek 1,2, Agnieszka Wnęk 1, Maria Zbylut 1, Waldemar Popiński 3 1) Environmental Engineering and Land Surveying Department, University of Agriculture
Wiesław Kosek 1,2, Agnieszka Wnęk 1, Maria Zbylut 1, Waldemar Popiński 3 1) Environmental Engineering and Land Surveying Department, University of Agriculture
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Geodetic Deformation, Seismicity and Fault Friction Ge277- 2007 Sensitivity of seismicity to stress perturbations, implications for earthquakes nucleation
Geodetic Deformation, Seismicity and Fault Friction Ge277- 2007 Sensitivity of seismicity to stress perturbations, implications for earthquakes nucleation
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