Verification of RASS-measured temperature profiles using a radio-controlled model glider     

John R. Taylor  Nathan J. Segal  Michael R. Bradshaw  David J. Low 《Meteorology and Atmospheric Physics》2013,119(3-4):197-206

Potential sonic temperature profiles from a continuous electromagnetic, pulsed acoustic, radio acoustic sounding system (RASS) were compared with profiles recorded by a commercially available temperature, relative humidity and pressure recorder mounted in a radio-controlled model motor-glider. The glider profiles covered the period of the morning transition in the lowest 200 m of an initially stably stratified boundary layer. Comparison of the profiles shows that the sonic temperature can be calculated based on the average speed of sound in the boundary layer; this removes the need to correct for vertical velocity in each temperature profile, thus avoiding the possibility of contaminating the temperatures with measurement noise from the vertical velocity profiles. Further, the low-level cold bias that occurs with the spatially separated transmit and receive antennas of a bistatic RASS system was not significant for the present measurements as the separation between the antennas was minimised. The comparison of RASS and glider temperatures gives confidence in the use of RASS-derived temperatures for investigating the performance of boundary layer models.  相似文献   

Influence of road network and population demand assumptions in evacuation modeling for distant tsunamis     

Kevin D. Henry  Nathan J. Wood  Tim G. Frazier 《Natural Hazards》2017,85(3):1665-1687

Tsunami evacuation planning in coastal communities is typically focused on local events where at-risk individuals must move on foot in a matter of minutes to safety. Less attention has been placed on distant tsunamis, where evacuations unfold over several hours, are often dominated by vehicle use and are managed by public safety officials. Traditional traffic simulation models focus on estimating clearance times but often overlook the influence of varying population demand, alternative modes, background traffic, shadow evacuation, and traffic management alternatives. These factors are especially important for island communities with limited egress options to safety. We use the coastal community of Balboa Island, California (USA), as a case study to explore the range of potential clearance times prior to wave arrival for a distant tsunami scenario. We use a first-in–first-out queuing simulation environment to estimate variations in clearance times, given varying assumptions of the evacuating population (demand) and the road network over which they evacuate (supply). Results suggest clearance times are less than wave arrival times for a distant tsunami, except when we assume maximum vehicle usage for residents, employees, and tourists for a weekend scenario. A two-lane bridge to the mainland was the primary traffic bottleneck, thereby minimizing the effect of departure times, shadow evacuations, background traffic, boat-based evacuations, and traffic light timing on overall community clearance time. Reducing vehicular demand generally reduced clearance time, whereas improvements to road capacity had mixed results. Finally, failure to recognize non-residential employee and tourist populations in the vehicle demand substantially underestimated clearance time.  相似文献   

Effect of Ni2+, Zn2+, and Co2+ on green rust transformation to magnetite     

Farr  Orion  Elzinga  Evert J.  Yee  Nathan 《Geochemical transactions》2022,23(1):1-25

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The city of Tyre,Lebanon and its semi-artificial tombolo     

Yaacov Nir 《Geoarchaeology》1996,11(3):235-250

The sedimentological history of the peninsular city of Tyre, located on the southern coast of Lebanon, reflects the political events surrounding Alexander the Great's conquest of the East (332 B.C.E.). Like many other Phoenician settlements, the city was originally situated on a small, relict rocky islet, but was later connected to the mainland by an artificial causeway constructed by Alexander's troops. As a result of the causeway construction, a gigantic tombolo formed, composed of at least 10 million m³ of sediment, mostly sand. Calculations based on the present size of the land tombolo of Tyre show that the average regional yearly volume of sand drift from the south and the north for the past 2300 years was approximately 4000 m³. If the present composition of high carbonate tombolo sands is representative of the entire sand body of the tombolo, about two thirds of the mass originates from nearby beaches which formed as a result of the erosion of the Pleistocene carbonate sandstone known as “Hajar Ramli.” © 1996 John Wiley & Sons, Inc.  相似文献