A National Operational Wave Observation Plan An Integrated Ocean Observing System plan for a comprehensive, high quality surface-wave monitoring network for the United States, which addresses the requirements of the mari

Source URL: cdn.ioos.noaa.gov

Surface properties of chiral d-wave superconductor with hexagonal symmetry Jun Goryo, Department of Mathematics and Physics, Hirosaki University Abstract: Surface properties are examined in a chiral d-wave (dx2-y2+idxy -

Source URL: www.physics.okayama-u.ac.jp

Kevin’s Flowers Flowers in the garden, the park, and the wild are all bright stars in a wave of energy that has been traveling around the globe since the first humans set foot on the Planet’s surface. Flowers are pil

Source URL: www.kevinwoodson.com

Geophys. J. Int, 1239–1260 doi: j.1365-246Xx Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements

Source URL: ciei.colorado.edu

UCRL-JCExt Abs Surface Wave Research in the Middle East and North Africa Michael E. Pasyanos and William R. Walter

Source URL: profile.usgs.gov

Specification for Sea State Preamble/Introduction. Waves are generated by ocean surface vector stress and evolve from wind waves to swell when the stress has insufficient magnitude to support the waves. Wave characterist

Source URL: ioc-goos-oopc.org

PARAMETERIZATION OF A WAVE-DEPENDENT SURFACE ROUGHNESS: A STEP TOWARDS A FULLY COUPLED ATMOSPHERE-OCEAN-SEA ICE-WAVE SYSTEM Elodie Charles1 and Mark Hemer1 1 Centre for Australian Weather and Climate Research:

Source URL: www.waveworkshop.org

Helmholtz surface wave tomography for isotropic and azimuthally anisotropic structure

Source URL: noise.earth.utah.edu

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Source URL: easd.geosc.uh.edu

• Seismology
• Mechanics
• Wave mechanics
• Petroleum geology
• Elasticity
• Geophysics
• Seismic anisotropy
• Physics
• Anisotropy
• Shear wave splitting
• Surface wave
• Seismic wave

Specification for Ocean Surface Vector Stress (OSVS) Preamble/Introduction. Ocean surface vector stress (OSVS) is also the drag at the bottom of the atmosphere and the dynamical forcing at the top of the ocean. OSVS is t

Source URL: ioc-goos-oopc.org

• Physical geography
• Oceanography
• Physical oceanography
• Earth
• Ocean observations
• Global Climate Observing System
• GOOS
• Mixed layer
• Meteorology
• Wind wave model
• Ocean current
• Climate