Climate 2010 Gary Strand High Performance Network Planning Workshop.
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Transcript of Climate 2010 Gary Strand High Performance Network Planning Workshop.
![Page 1: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/1.jpg)
Climate 2010
Gary Strand
High Performance Network Planning Workshop
![Page 2: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/2.jpg)
Climate 2010The past
• Two, sometimes three components• Low resolution, spatially and temporally
– Atmosphere• ~500 - 800 km grid (think Montana), 9 vertical levels
– Ocean• 200 km by 200 km grid (1/2 Maine), 20 vertical levels
– Sea ice (maybe)• Same grid as ocean, simple dynamics
• 100 years of model time is ~50 Gigabytes• Data distribution uncommon, slow, and painful
![Page 3: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/3.jpg)
Climate 2010The present
• ~Four interactive components• Higher resolution, spatially and temporally
– Atmosphere• 230 km grid (W Virginia), 18 vertical levels
– Ocean• 100 km grid (2x Delaware), 40 vertical levels
– Sea ice • Same as ocean grid, fully dynamic
– Land surface• Same grid as atmosphere
• 100 years of model time is ~1 Terabyte• Data distribution common, ESG will help
![Page 4: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/4.jpg)
Climate 20105 years from now
• Five or more interactive components• Still higher resolution, spatially and temporally
– Atmosphere• 30 km grid (4x DC), 60 vertical levels
– Ocean• 10 km grid (1/2 DC), 40 vertical levels
– Sea ice • 10 km grid, or less
– Land surface model, fully dynamic vegetation– Carbon cycle model– Atmospheric chemistry– Preliminary observational data assimilation
• 100 years of model time is ~100 TB• Data distribution common, pain free
![Page 5: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/5.jpg)
Climate in 2010• Several (six, seven?) interactive components• Yet still higher resolution, spatially and temporally
– Atmosphere, ocean, sea ice – Fully dynamic vegetation– Carbon cycle– Atmospheric chemistry– Biochemistry– Full assimilation of observational data– Econometric models– Population growth and land use change models– Solar processes
• 100 years of model time is at least ~1/2 PB• Widespread data distribution mandatory
![Page 6: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/6.jpg)
Climate in 2010
A graphic illustration
![Page 7: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/7.jpg)
Climate in 2010
And one more…
![Page 8: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/8.jpg)
Climate 2010Conclusions
• Climate models have evolved steadily, but that evolution will become more rapid in the future
• Generated data volumes have, and will, increase exponentially
• Widespread data distribution is required for analysis, visualization, and assessment
…All of which mean:• All aspects of network infrastructure must keep
up if the science is to progress
![Page 9: Climate 2010 Gary Strand High Performance Network Planning Workshop.](https://reader036.fdocuments.net/reader036/viewer/2022083009/56649e5e5503460f94b57ab3/html5/thumbnails/9.jpg)
Climate 2010
The End