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Olympic Peninsula
Lazed and Diffused: Untangling Noble Gas Thermochronometry Data for Exhumation Rates
Autopsy of a reservoir: Facies architecture in a multidam system, Elwha River, Washington, USA
Repeated megaturbidite deposition in Lake Crescent, Washington, USA, triggered by Holocene ruptures of the Lake Creek-Boundary Creek fault system
Tectonic and glacial contributions to focused exhumation in the Olympic Mountains, Washington, USA
Age and volcanic stratigraphy of the Eocene Siletzia oceanic plateau in Washington and on Vancouver Island
Shallow geophysical imaging of the Olympia anomaly: An enigmatic structure in the southern Puget Lowland, Washington State
Paleoseismic Evidence for Late Holocene Tectonic Deformation along the Saddle Mountain Fault Zone, Southeastern Olympic Peninsula, Washington
Western limits of the Seattle fault zone and its interaction with the Olympic Peninsula, Washington
Watching the Wind: Seismic Data Contamination at Long Periods due to Atmospheric Pressure‐Field‐Induced Tilting
Spatially heterogeneous burial and high- P / T metamorphism in the Crescent Formation, Olympic Peninsula, Washington
Saddle Mountain fault deformation zone, Olympic Peninsula, Washington: Western boundary of the Seattle uplift
Two Post-Glacial Earthquakes on the Saddle Mountain West Fault, Southeastern Olympic Peninsula, Washington
PLEISTOCENE WALRUS HERDS IN THE OLYMPIC PENINSULA AREA: TRACE-FOSSIL EVIDENCE OF PREDATION BY HYDRAULIC JETTING
This paper presents a review of recent progress on the theory of orographic precipitation and a discussion of the role of preexisting atmospheric disturbances, especially their strong water vapor fluxes. I also introduce the basic elements of stable moist airflow dynamics and cloud physics, and a new linear theory of orographic precipitation. The theory is tested against two types of data: a single event of Alpine precipitation and the annual climatology of the Oregon coastal ranges. Different methods are used to determine the free “cloud-delay” parameters in the theory, including a statistical analysis of data from conventional rain gauges and isotope analysis of stream samples. The surprising threshold behavior of nonlinear accretion-dominated cloud physics is displayed. Finally, I consider the impact of scale-dependent precipitation patterns on erosion and terrain evolution.