NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
A High-Resolution Merged Wind Dataset for DYNAMO: Progress and Future PlansIn order to support research on optimal data assimilation methods for the Cyclone Global Navigation Satellite System (CYGNSS), launching in 2016, work has been ongoing to produce a high‐resolution merged wind dataset for the Dynamics of the Madden Julian Oscillation (DYNAMO) field campaign, which took place during late 2011/early 2012. The winds are produced by assimilating DYNAMO observations into the Weather Research and Forecasting (WRF) three‐dimensional variational (3DVAR) system. Data sources from the DYNAMO campaign include the upper‐air sounding network, radial velocities from the radar network, vector winds from the Advanced Scatterometer (ASCAT) and Oceansat‐2 Scatterometer (OSCAT) satellite instruments, the NOAA High Resolution Doppler Lidar (HRDL), and several others. In order the prep them for 3DVAR, significant additional quality control work is being done for the currently available TOGA and SMART‐R radar datasets, including automatically dealiasing radial velocities and correcting for intermittent TOGA antenna azimuth angle errors. The assimilated winds are being made available as model output fields from WRF on two separate grids with different horizontal resolutions ‐ a 3‐km grid focusing on the main DYNAMO quadrilateral (i.e., Gan Island, the R/V Revelle, the R/V Mirai, and Diego Garcia), and a 1‐km grid focusing on the Revelle. The wind dataset is focused on three separate approximately 2‐week periods during the Madden Julian Oscillation (MJO) onsets that occurred in October, November, and December 2011. Work is ongoing to convert the 10‐m surface winds from these model fields to simulated CYGNSS observations using the CYGNSS End‐To‐End Simulator (E2ES), and these simulated satellite observations are being compared to radar observations of DYNAMO precipitation systems to document the anticipated ability of CYGNSS to provide information on the relationships between surface winds and oceanic precipitation at the mesoscale level. This research will improve our understanding of the future utility of CYGNSS for documenting key MJO processes.
Document ID
20150002896
Acquisition Source
Marshall Space Flight Center
Document Type
Abstract
Authors
Lang, Timothy J.
(NASA Marshall Space Flight Center Huntsville, AL, United States)
Mecikalski, John
(Alabama Univ. Huntsville, AL, United States)
Li, Xuanli
(Alabama Univ. Huntsville, AL, United States)
Chronis, Themis
(Alabama Univ. Huntsville, AL, United States)
Castillo, Tyler
(Alabama Univ. Huntsville, AL, United States)
Hoover, Kacie
(Alabama Univ. Huntsville, AL, United States)
Brewer, Alan
(National Oceanic and Atmospheric Administration Washington, DC, United States)
Churnside, James
(National Oceanic and Atmospheric Administration Washington, DC, United States)
McCarty, Brandi
(National Oceanic and Atmospheric Administration Washington, DC, United States)
Hein, Paul
(Colorado State Univ. Fort Collins, CO, United States)
Rutledge, Steve
(Colorado State Univ. Fort Collins, CO, United States)
Dolan, Brenda
(Colorado State Univ. Fort Collins, CO, United States)
Matthews, Alyssa
(Colorado State Univ. Fort Collins, CO, United States)
Thompson, Elizabeth
(Colorado State Univ. Fort Collins, CO, United States)
Date Acquired
March 13, 2015
Publication Date
January 4, 2015
Subject Category
Meteorology And Climatology
Earth Resources And Remote Sensing
Report/Patent Number
M14-3970
Report Number: M14-3970
Meeting Information
Meeting: American Meteorological Society (AMS) Annual Meeting
Location: Phoenix, AZ
Country: United States
Start Date: January 4, 2015
End Date: January 8, 2015
Sponsors: American Meteorological Society
Distribution Limits
Public
Copyright
Public Use Permitted.
No Preview Available