Upper-atmospheric models: Difference between revisions
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Cjnankervis (talk | contribs) Process used to generate seasonal weather forecasts using upper atmosphere jet stream modelling |
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Most [[climate models]] simulate a region of the Earth's atmosphere from the surface to the [[stratopause]]. There also exist numerical models which simulate the wind, temperature and composition of the Earth's tenuous [[upper atmosphere]], from the [[mesosphere]] to the [[exosphere]], including the [[ionosphere]]. This region is affected strongly by the 11 year [[Solar cycle]] through variations in solar UV/EUV/Xray radiation and [[solar wind]] leading to high latitude particle precipitation and [[Aurora (astronomy)|aurora]]. It has been proposed that these phenomena may have an effect on the lower atmosphere, and should therefore be included in simulations of climate change. For this reason there has been a drive in recent years to create "whole atmosphere" models to investigate whether or not this is the case. |
Most [[climate models]] simulate a region of the Earth's atmosphere from the surface to the [[stratopause]]. There also exist numerical models which simulate the wind, temperature and composition of the Earth's tenuous [[upper atmosphere]], from the [[mesosphere]] to the [[exosphere]], including the [[ionosphere]]. This region is affected strongly by the 11 year [[Solar cycle]] through variations in solar UV/EUV/Xray radiation and [[solar wind]] leading to high latitude particle precipitation and [[Aurora (astronomy)|aurora]]. It has been proposed that these phenomena may have an effect on the lower atmosphere, and should therefore be included in simulations of climate change. For this reason there has been a drive in recent years to create "whole atmosphere" models to investigate whether or not this is the case. |
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A [[jet stream]] perturbation model is employed by Weather Logistics UK<ref name="Weather Logistics UK">{{Citation|url='http://www.weatherlogistics.com/wordpress/?p=740' |title=overview of jet-stream / blocking interaction model, March 2011}}</ref>, which simulates the diversion of the air streams in the [[upper atmosphere]]. [[North Atlantic]] air flow modelling is simulated by combining a monthly [[jet stream|jet stream]] climatology input calculated at 20 to 30°W, with different [[Block (meteorology)|blocking high patterns]]. The jet stream input is generated by [[thermal wind balance]] calculations at 316mbars (~6 - 9km aloft) in the mid-latitude range from 40 to 60°N. Long term blocking patterns are determined by the [[weather forecaster]], who identifies the likely position and strength of North Atlantic [[Block (meteorology)|Highs]] from [[synoptic charts]], the [[North Atlantic Oscillation]] (NAO) and [[El Niño-Southern Oscillation]] (ENSO) patterns. The model is based on the knowledge that low pressure systems at the surface are steered by the fast ribbons (jet streams) of air in the [[upper atmosphere]]. The jet stream - blocking interaction model simulation examines the sea [[Sea surface temperature|surface temperature]] field using data from [[National Oceanic and Atmospheric Administration|NOAA]] tracked along the ocean on a path to the British Isles. The principal theory suggests that long term weather patterns act on longer time scales, so large blocking patterns are thought to appear in a similar locations repeatedly over several months<ref name="Weather Logistics UK - Seasonal forecasting">{{Citation|url='http://www.weatherlogistics.com/Seasonal.pdf' |title=The Technophobes Guide to Seasonal Forecasting in the 21st Century, August 2009}}</ref>. With a good knowledge of blocking high patterns, the model performs with an impressive accuracy that is useful to the end user<ref name="Weather Logistics UK Validation">{{Citation|url='http://www.weatherlogistics.com/Software_Outputsv3.pdf' |title=validation of jet-stream / blocking model, Winter 2010/2011 (Version 3)}}</ref>. |
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The modelling undertaken at Weather Logistics UK produces regional-seasonal predictions that are [[Probabilistic forecasting|probabilistic]] in nature. Two different blocking sizes are used for the modelling, located at two different locations. The four possible blocking diversions are then ranked in an order, to be combined by [[logistic regression]] and generate the appropriate likelihoods of weather events on seasonal time-scales. The raw output consists of 22 different weather conditions for each season. Each of the outcomes are assumed to occur with equal likelihood over a sufficiently long (climate) time scale. The seasonal outputs are therefore compared average blocking scenario. A [[global warming bias]] and 1961-1990 [[Climate of the United Kingdom|climatology]] of regional British Isles temperatures are added to the anomaly value to produce a final temperature prediction. The seasonal weather forecasts at Weather Logistics UK<ref name="Weather Logistics UK">{{Citation|url='http://www.weatherlogistics.com/wordpress/?p=740' |title=overview of jet-stream / blocking model}}</ref> comprise of several additional weather components (derivatives) including: precipitation, storminess, air flow trajectories, [[Heating degree day|heating degree days]] for household utility bills, cooling degree days, [[Heat wave|heat wave]] and [[Weather-related cancellation|snow days]] odds. |
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== External links == |
== External links == |
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Four examples of upper atmospheric models are |
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* [http://www.hao.ucar.edu/modeling/tgcm NCAR TIE-GCM (97 to ~450km), NCAR TIME-GCM (30 to ~450km)] |
* [http://www.hao.ucar.edu/modeling/tgcm NCAR TIE-GCM (97 to ~450km), NCAR TIME-GCM (30 to ~450km)] |
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* [http://www.apl.ucl.ac.uk/research/modelling.html UCL CTIP (80km to ~ 450km), UCL CMAT (30km to ~ 450km)] |
* [http://www.apl.ucl.ac.uk/research/modelling.html UCL CTIP (80km to ~ 450km), UCL CMAT (30km to ~ 450km)] |
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* [http://www.uam.mstu.edu.ru/index.php/Welcome_to_UAM UAM is the global mathematical model of the Earth's upper atmosphere (mesosphere, thermosphere, ionosphere, plasmasphere and inner magnetosphere). ] |
* [http://www.uam.mstu.edu.ru/index.php/Welcome_to_UAM UAM is the global mathematical model of the Earth's upper atmosphere (mesosphere, thermosphere, ionosphere, plasmasphere and inner magnetosphere). ] |
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* [http://www.weatherlogistics.com/wordpress/?p=740 Weather Logistics UK: Jet stream - Blocking interaction model (5 to 9km) jet stream - blocking diversion model to simulate large scale and long term air flow for the British Isles. Incorporates sea surface temperature data from NOAA and a monthly jet stream climatology. ] |
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== References == |
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{{Reflist}} |
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An example of a whole atmosphere model is |
An example of a whole atmosphere model is |
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Revision as of 16:13, 12 April 2011
Most climate models simulate a region of the Earth's atmosphere from the surface to the stratopause. There also exist numerical models which simulate the wind, temperature and composition of the Earth's tenuous upper atmosphere, from the mesosphere to the exosphere, including the ionosphere. This region is affected strongly by the 11 year Solar cycle through variations in solar UV/EUV/Xray radiation and solar wind leading to high latitude particle precipitation and aurora. It has been proposed that these phenomena may have an effect on the lower atmosphere, and should therefore be included in simulations of climate change. For this reason there has been a drive in recent years to create "whole atmosphere" models to investigate whether or not this is the case.
A jet stream perturbation model is employed by Weather Logistics UK[1], which simulates the diversion of the air streams in the upper atmosphere. North Atlantic air flow modelling is simulated by combining a monthly jet stream climatology input calculated at 20 to 30°W, with different blocking high patterns. The jet stream input is generated by thermal wind balance calculations at 316mbars (~6 - 9km aloft) in the mid-latitude range from 40 to 60°N. Long term blocking patterns are determined by the weather forecaster, who identifies the likely position and strength of North Atlantic Highs from synoptic charts, the North Atlantic Oscillation (NAO) and El Niño-Southern Oscillation (ENSO) patterns. The model is based on the knowledge that low pressure systems at the surface are steered by the fast ribbons (jet streams) of air in the upper atmosphere. The jet stream - blocking interaction model simulation examines the sea surface temperature field using data from NOAA tracked along the ocean on a path to the British Isles. The principal theory suggests that long term weather patterns act on longer time scales, so large blocking patterns are thought to appear in a similar locations repeatedly over several months[2]. With a good knowledge of blocking high patterns, the model performs with an impressive accuracy that is useful to the end user[3].
The modelling undertaken at Weather Logistics UK produces regional-seasonal predictions that are probabilistic in nature. Two different blocking sizes are used for the modelling, located at two different locations. The four possible blocking diversions are then ranked in an order, to be combined by logistic regression and generate the appropriate likelihoods of weather events on seasonal time-scales. The raw output consists of 22 different weather conditions for each season. Each of the outcomes are assumed to occur with equal likelihood over a sufficiently long (climate) time scale. The seasonal outputs are therefore compared average blocking scenario. A global warming bias and 1961-1990 climatology of regional British Isles temperatures are added to the anomaly value to produce a final temperature prediction. The seasonal weather forecasts at Weather Logistics UK[1] comprise of several additional weather components (derivatives) including: precipitation, storminess, air flow trajectories, heating degree days for household utility bills, cooling degree days, heat wave and snow days odds.
External links
Four examples of upper atmospheric models are
- NCAR TIE-GCM (97 to ~450km), NCAR TIME-GCM (30 to ~450km)
- UCL CTIP (80km to ~ 450km), UCL CMAT (30km to ~ 450km)
- UAM is the global mathematical model of the Earth's upper atmosphere (mesosphere, thermosphere, ionosphere, plasmasphere and inner magnetosphere).
- Weather Logistics UK: Jet stream - Blocking interaction model (5 to 9km) jet stream - blocking diversion model to simulate large scale and long term air flow for the British Isles. Incorporates sea surface temperature data from NOAA and a monthly jet stream climatology.
References
- ^ a b ['http://www.weatherlogistics.com/wordpress/?p=740' overview of jet-stream / blocking interaction model, March 2011]
{{citation}}: Check|url=value (help) Cite error: The named reference "Weather Logistics UK" was defined multiple times with different content (see the help page). - ^ ['http://www.weatherlogistics.com/Seasonal.pdf' The Technophobes Guide to Seasonal Forecasting in the 21st Century, August 2009]
{{citation}}: Check|url=value (help) - ^ ['http://www.weatherlogistics.com/Software_Outputsv3.pdf' validation of jet-stream / blocking model, Winter 2010/2011 (Version 3)]
{{citation}}: Check|url=value (help)
An example of a whole atmosphere model is
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