Asset Details
MbrlCatalogueTitleDetail
Do you wish to reserve the book?
Near-Surface Density Currents Observed in the Southeast Pacific Stratocumulus-Topped Marine Boundary Layer
by
Yuter, Sandra E.
, de Szoeke, Simon P.
, Hall, Andrew M.
, Burleyson, Casey D.
, Miller, Matthew A.
, Wilbanks, Matt C.
, Brewer, W. Alan
in
Boundary layers
/ Clouds
/ Cold
/ Density
/ Density currents
/ Doppler effect
/ Drying
/ Evaporation
/ Lidar
/ Marine
/ Meteorology
/ Pools
/ Rain
/ Similarity
/ Stratocumulus clouds
/ Studies
2015
Hey, we have placed the reservation for you!
By the way, why not check out events that you can attend while you pick your title.
You are currently in the queue to collect this book. You will be notified once it is your turn to collect the book.
Oops! Something went wrong.
Looks like we were not able to place the reservation. Kindly try again later.
Are you sure you want to remove the book from the shelf?
Near-Surface Density Currents Observed in the Southeast Pacific Stratocumulus-Topped Marine Boundary Layer
by
Yuter, Sandra E.
, de Szoeke, Simon P.
, Hall, Andrew M.
, Burleyson, Casey D.
, Miller, Matthew A.
, Wilbanks, Matt C.
, Brewer, W. Alan
in
Boundary layers
/ Clouds
/ Cold
/ Density
/ Density currents
/ Doppler effect
/ Drying
/ Evaporation
/ Lidar
/ Marine
/ Meteorology
/ Pools
/ Rain
/ Similarity
/ Stratocumulus clouds
/ Studies
2015
Oops! Something went wrong.
While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Near-Surface Density Currents Observed in the Southeast Pacific Stratocumulus-Topped Marine Boundary Layer
by
Yuter, Sandra E.
, de Szoeke, Simon P.
, Hall, Andrew M.
, Burleyson, Casey D.
, Miller, Matthew A.
, Wilbanks, Matt C.
, Brewer, W. Alan
in
Boundary layers
/ Clouds
/ Cold
/ Density
/ Density currents
/ Doppler effect
/ Drying
/ Evaporation
/ Lidar
/ Marine
/ Meteorology
/ Pools
/ Rain
/ Similarity
/ Stratocumulus clouds
/ Studies
2015
Please be aware that the book you have requested cannot be checked out. If you would like to checkout this book, you can reserve another copy
We have requested the book for you!
Your request is successful and it will be processed during the Library working hours. Please check the status of your request in My Requests.
Oops! Something went wrong.
Looks like we were not able to place your request. Kindly try again later.
Near-Surface Density Currents Observed in the Southeast Pacific Stratocumulus-Topped Marine Boundary Layer
Journal Article
Near-Surface Density Currents Observed in the Southeast Pacific Stratocumulus-Topped Marine Boundary Layer
2015
Request Book From Autostore
and Choose the Collection Method
Overview
Density currents (i.e., cold pools or outflows) beneath marine stratocumulus clouds are characterized using 30 days of ship-based observations obtained during the 2008 Variability of American Monsoon Systems (VAMOS) Ocean–Cloud–Atmosphere–Land Study Regional Experiment (VOCALS-REx) in the southeast Pacific. An air density increase criterion applied to the Improved Meteorological (IMET) sensor data identified 71 density current front, core (peak density), and tail (dissipating) zones. The similarity in speeds of the mean density current propagation speed (1.8 m s−1) and the mean cloud-level advection relative to the surface layer wind (1.9 m s−1) allowed drizzle cells to deposit elongated density currents in their wakes. Scanning Doppler lidar captured prefrontal updrafts with a mean intensity of 0.91 m s−1 and an average vertical extent of 800 m. Updrafts were often surmounted by low-lying shelf clouds not connected to the overlying stratocumulus cloud. The observed density currents were 5–10 times thinner and weaker than typical continental thunderstorm cold pools. Nearly 90% of density currents were identified when C-band radar estimated areal average rain rates exceeded 1 mm day−1 over a 30-km diameter. Rather than peaking when rain rates were highest overnight, density current occurrence peaks between 0600 and 0800 local solar time when enhanced local drizzle co-occurred with shallow subcloud dry and stable layers. The dry layers may have contributed to density current formation by enhancing subcloud evaporation of drizzle. Density currents preferentially occurred in a large region of predominantly open cells but also occurred in regions of closed cells.
MBRLCatalogueRelatedBooks
Related Items
Related Items
We currently cannot retrieve any items related to this title. Kindly check back at a later time.
This website uses cookies to ensure you get the best experience on our website.