Examples of DRILSDOWN projects

Basic Examples

Atmospheric (observed): What do clouds look like where they are acting to increase the water vapor?

One example of “drilling down” is to view satellite imagery around places where interesting quantitative meteorology is diagnosed. (This example)[https://github.com/Unidata/drilsdown/tree/master/UseCase_Examples/WaterVaporTendencies] constructs URLs to a NASA imagery server, from the date and time information around extreme values of a Lagrangian water vapor tendency.

The next level of scientific inquiry here is to call up a vertical sounding display, from a global 3D meteorological analysis, in either the IDV or a Jupyter Python session.

These headers within the .ipynb notebook may help clarify the workflow:

Atmospheric (observed): How do watervapor “islands” last long over the dry western-equatorial Indian Ocean?

Over the western equatorial Indian ocean, which is usually dry, there are occasional periods when filaments or “islands” of water vapor in the atmopshere are brought by the winds. These last surprisingly long, even as rain acts to remove the vapor. We wanted to study several such instances using vertical profile probes and column water vapor maps over region bounded by 17, 36 ; -15, 90 (North , West ; South, East).

A list of begin and end dates was supplied by by Dr. Matt Igel of UC-Davis, based on his blob-tracking results applied to column water vapor (CWV).

A script is generated to teleport the simple IDV bundle to a zidv bundle comprising of 3D data from two reanalysis for the lat-lon bounding box 17 - 36 , -15 - 90 (North - West ,South - East).

Generated teleport bash script was run in a headless linux environment to generate zidv files. These zidv case files are then published to RAMADDA server using following command:

ramadda_publish 'Igel_WEIO*.zidv' a4154517-ac1c-4eb4-b842-572cb55ce1f2 -a 'Igel_WEIO*.gif' -username user -password pass

Links for these command line utilities: IDV_teleport , RAMADDA_publish

Atmospheric (complex, simulated): What is going on in areas where small scales are adding energy to the large-scale flow?

In this project, a global model with 7km mesh produced an enormous dataset including vertical flux of horizontal momentum (u’w’ and v’w’). The notebooks below show some “drilling down” results.

These headers within two of the .ipynb notebooks in examples/MomentumFlux_in_GlobalCloudmodel show the workflow:

Oceanic: What’s going on when the Loop Current in the Gulf of Mexico splits off an eddy?