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Pastimes : Bridging weather and climate

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To: weatherguru who wrote (145)4/1/2016 8:01:13 AM
From: FJB1 Recommendation

Recommended By
TideGlider

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Thought you might like this cool map. Can't vouch for its accuracy or anything. It is just pretty.

earth.nullschool.net

earth.nullschool.net

earth - a visualization of global weather conditions


a visualization of global weather conditions

forecast by supercomputers

updated every three hours



ocean surface current estimates

updated every five days



ocean surface temperatures and

anomaly from daily average (1981-2011)

updated daily




ocean waves

updated every three hours

purchase artwork from Point.B Studio to help support this site

Community |

Facebook Page

Author |

Cameron Beccario @cambecc

Free Version of Source |

github.com/cambecc/earth

Modules |

D3.js, backbone.js, when.js, node.js

Weather Data |

GFS (Global Forecast System)
NCEP / National Weather Service / NOAA

Ocean Currents Data |

OSCAR
Earth & Space Research

Sea Surface Temperature |

Real Time Global SST
MMAB / EMC / NCEP

Waves |

WAVEWATCH III
MMAB / EMC / NCEP

Aerosols and Chemistry |

GEOS-5 (Goddard Earth Observing System)
GMAO / NASA

GRIB/NetCDF Decoder |

UCAR/Unidata THREDDS

Geographic Data |

Natural Earth

Hosting |

CloudFlare, Amazon S3

Font |

M+ FONTS, Mono Social Icons Font

Color Scales |

chroma.js
ColorBrewer2.org
Kindlmann Linear Luminance
MYCARTA
Dave Green's cubehelix

Waterman Butterfly |

watermanpolyhedron.com

Earlier Work |

Tokyo Wind Map

Inspiration |

HINT.FM wind map

atmospheric pressure corresponds roughly to altitude

several pressure layers are meteorologically interesting

they show data assuming the earth is completely smooth

note: 1 hectopascal (hPa) = 1 millibar (mb)

1000 hPa |

~100 m, near sea level conditions

850 hPa |

~1,500 m, planetary boundary, low

700 hPa |

~3,500 m, planetary boundary, high

500 hPa |

~5,000 m, vorticity

250 hPa |

~10,500 m, jet stream

70 hPa |

~17,500 m, stratosphere

10 hPa |

~26,500 m, even more stratosphere

the "Surface" layer represents conditions at ground or water level

this layer follows the contours of mountains, valleys, etc.



overlays show another dimension of data using color

some overlays are valid at a specific height

while others are valid for the entire thickness of the atmosphere

Wind |

wind speed at specified height

Temp |

temperature at specified height

TPW ( Total Precipitable Water) |

total amount of water in a column of air
stretching from ground to space

RH |

relative humidity at specified height

WPD ( Wind Power Density) |

measure of power available in the wind

TCW (Total Cloud Water) |

total amount of water in clouds
in a column of air from ground to space

MSLP ( Mean Sea Level Pressure) |

air pressure reduced to sea level

MI (Misery Index) |

perceived air temperature
combined heat index and wind chill

SST (Sea Surface Temp) |

temperature of the ocean surface

SSTA (Sea Surface Temp Anomaly) |

difference in ocean temperature from
daily average during years 1981-2011

Peak Wave Period |

period of most energetic waves,
whether swells or wind generated

HTSGW ( Significant Wave Height) |

roughly equal to mean wave height
as estimated by a "trained observer"

COsc (CO Surface Concentration) |

the fraction of carbon monoxide present
in air at the earth's surface

CO2sc (CO2 Surface Concentration) |

the fraction of carbon dioxide present
in air at the earth's surface

SO2sm (Sulfur Dioxide Surface Mass) |

amount of sulfur dioxide in the air near
the earth's surface

DUext (Dust Extinction) |

the aerosol optical thickness (AOT) of
light at 550 nm due to dust

SO4ext (Sulfate Extinction) |

the aerosol optical thickness (AOT) of
light at 550 nm due to sulfate

about ocean waves

Significant Wave Height is the average height of the highest 1/3 of waves at a particular point in the ocean. There's a great writeup here describing what this means.

Peak Wave Period is the (inverse) frequency of the most energetic waves passing through a particular point, whether wind generated or swells. Certainly, there are many more groups of waves moving through an area, each in different directions, but trying to show them all rapidly becomes complex. Instead, we show the one wave group contributing the most energy. This has the effect, though, of creating "boundaries" between regions of ocean where the #1 wave group suddenly switches to second place. Often these boundaries represent swell fronts, but other times they are just artifacts of the ranking mechanism.

about CO2 concentrations

While implementing the visualization of CO2 surface concentration, I noticed the NASA GEOS-5 model reports a global mean concentration that differs significantly from widely reported numbers. For example, from the run at 2015-11-23 00:00 UTC, the global mean is only 368 ppmv whereas CO2 observatories report concentrations closer to 400 ppmv. GEOS-5 was constructed in the 2000s, so perhaps the model does not account for accumulation of atmospheric CO2 over time? This is simply speculation. I'm just not certain.

To bring the GEOS-5 results closer to contemporary numbers, I have added a uniform offset of +32 ppmv, increasing the global mean to 400 ppmv. This is not scientifically valid, but it does allow the visualization to become illustrative of the discussion occurring today around atmospheric CO2. Without question, I would welcome a more rigorous approach or an explanation why the GEOS-5 model produces the data that it does.

disclaimer

GEOS-5 data (covering all Chem and Particulates layers) comes with the following disclaimer: Forecasts using the GEOS system are experimental and are produced for research purposes only. Use of these forecasts for purposes other than research is not recommended.
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