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The Langmuir Laboratory for Atmospheric Research is a scientific laboratory studying the cloud processes that produce lightning, hail, and rain, located in the Magdalena Mountains of central New Mexico. The lab is operated by the New Mexico Institute of Mining and Technology (New Mexico Tech) with funding from the National Science Foundation.
The Magdalena Ridge Observatory (MRO) is an astronomical observatory in Socorro County, New Mexico, about 32 kilometers (20 mi) west of the town of Socorro.The observatory is located in the Magdalena Mountains near the summit of South Baldy Mountain, adjacent to the Langmuir Laboratory for Atmospheric Research.
The Langmuir's location in the Magdalena Mountains was chosen "because thunderstorms are initiated by the mountains and the storms are often isolated, stationary, and relatively small" and occur with high frequency. Visiting scientists at Langmuir also study bats, hummingbirds, butterflies and plant life in the area. [5]
In 1943, the focus of Schaefer's and Langmuir's research shifted to precipitation static, aircraft icing, ice nuclei, and cloud physics, and many of their experiments were carried out at Mount Washington Observatory in New Hampshire. In the summer of 1946 Schaefer found his experimental "cold box" too warm for some laboratory tests he wanted to ...
Developments of PetDB [2] began in 1995, by Lamont–Doherty Earth Observatory (LDEO) [3] scientists C. Langmuir (now at Harvard University), W. Ryan, and A. Boulanger, when they realized what impact the World Wide Web and relational databases could have on the use of scientific data in research and in the classroom.
Educational observatory This is a partial list of astronomical observatories ordered by name, along with initial dates of operation (where an accurate date is available) and location. The list also includes a final year of operation for many observatories that are no longer in operation.
In physical oceanography, Langmuir circulation consists of a series of shallow, slow, counter-rotating vortices at the ocean's surface aligned with the wind. These circulations are developed when wind blows steadily over the sea surface.
The Langmuir adsorption model deviates significantly in many cases, primarily because it fails to account for the surface roughness of the adsorbent. Rough inhomogeneous surfaces have multiple site types available for adsorption, with some parameters varying from site to site, such as the heat of adsorption.