485 karma · joined April 15, 2014
https://www.weather.gov/hazstat
I'm not advocating for the personification of all extreme weather events, but the lethality of heatwaves is often overlooked.
Curiously, Shoeless Joe Jackson set a World Series hit record that was unbroken until 1964 and had the highest series batting average of either team. He also hit the only home run of the 1919 World Series.
Climate change is not a single event, nor a cluster of events, that occur(s) over a summer. Strong hurricanes have occurred well before Dorian [1]. So have heat waves [2].
Extreme weather happens. The change in the frequency of (some) extreme events can be attributed to anthropogenic climate change, but a single event cannot.
[1] https://en.wikipedia.org/wiki/1935_Labor_Day_hurricane
[2] https://en.wikipedia.org/wiki/1936_North_American_heat_wave
Also, an obligatory xkcd: https://xkcd.com/1168/
I surprised myself by remembering some symbols I haven't used in a while but was stumped on a few I should have known (nth roots).
Thankfully typesetting here meant math formulas, not minipage layouts.
MADIS is a bit dated, data dissemination that uses OPeNDAP [1] and ERDDAP [2] is much friendlier.
[0] https://github.com/Unidata/siphon
[1] https://opendap.github.io/documentation/
[2] https://coastwatch.pfeg.noaa.gov/erddap/information.html
Note these error statistics do not represent true model error as the official track and intensity forecast -- while informed by model output -- are determined by human forecasters.
For the interested, the ESRL Global Monitoring Division (https://www.esrl.noaa.gov/gmd/ccgg/index.html) is a more complete treatment of work being done in global greenhouse gas monitoring -- charts, maps and data included.
At each National Weather Service office, forecasters typically use model output to guide their daily forecast products, such as temperatures and precipitation probabilities. However, these forecasters are aware of smaller-scale nuances of their forecast area, such as topographic influences, land-sea interactions or urban heat island effects, which models may struggle to resolve. Human knowledge of model limitations helps to produce a better forecast.
A further example would be hurricane forecasting, where National Hurricane Center forecasts typically outperform most models (see http://www.nhc.noaa.gov/verification/verify6.shtml for starters).
Some examples of gravity waves in the atmosphere: [1] [2]
[0] http://glossary.ametsoc.org/wiki/Gravity_wave [1] http://cimss.ssec.wisc.edu/goes/blog/archives/2051 [2] https://www.youtube.com/watch?v=yXnkzeCU3bE
The program should begin at any time.
EDIT: Err, CET... UTC+1. So, perhaps it is over?
[0] http://science.ksc.nasa.gov/shuttle/missions/51-l/docs/roger...
http://www.cpc.ncep.noaa.gov/products/analysis_monitoring/en...
It would be interesting to see the station data integrated with an urban land cover map. Surface air temperature is sensitive to the locations of buildings, roads, soil type/water/ground cover, etc., not just elevation.