Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
| Authors: |
|
|
|---|---|---|
| Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
| Type: | Resource | |
| Storage: | The size of this resource is 201 bytes | |
| Created: | Jan 02, 2019 at 10:23 p.m. | |
| Last updated: | Feb 05, 2021 at 7:25 p.m. | |
| Citation: | See how to cite this resource |
| Sharing Status: | Public |
|---|---|
| Views: | 1535 |
| Downloads: | 4 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
Stable boundary layers are still a relatively problematic component of atmospheric modeling, despite their frequent occurrence. While general agreement exists that MO similarity is not applicable in the SBL due to the non-homogeneous, non-stationary flow, no universal organizing theory for the surface SBL has been presented. This poses a problem when examining aerosol movement as a function of atmospheric dynamics. It is known that stable air stratification results in katabatic downslope winds, even in very shallow topographic airsheds. These downslope winds can converge with background flow, and it is hypothesized that this convergence provides a starting point for specific events, such as internal gravity waves. Even though the stable boundary layer is normally shallow, internal gravity waves can propagate at an angle from the horizontal plane, and modify local shear, thus generating periodic turbulent mixing in space. Some studies have measured converging background and drainage flows in mountain areas, however, few studies have examined this in less dramatic, but more common, topographic areas. We are conducting a measurement campaign to address these open issues.
Raw DTS project data will be available in 2020 by contacting ctemps@unr.edu
Subject Keywords
Coverage
Spatial
Temporal
| Start Date: | |
|---|---|
| End Date: |
Content
readme.md
Basic components of study
DTS: Silixa Ultima
Cable: AFL Micro-DualPlenum Rated, 2 50μm BIF OM3 Laser-LinkTM 300 10 GB ethernet fibers, 2.0 mm, RoHS, Colored Fiber, White jacket color
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| National Science Foundation | Collaborative Research: Facility Support: Center for Transformative Environmental Monitoring Programs (CTEMPs) | 1440506 |
| National Science Foundation | 1733746 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
|---|---|---|---|---|
| CTEMPs OSU-UNR | CTEMPs | Nevada, US |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment