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Senast redigerad av censuria 2020-01-16 kl. 00:44.
Senast redigerad av censuria 2020-01-16 kl. 00:44.
. Jag förnekar inte att temperaturen stiger och koldioxiden mycket väl kan vara orsaken till det, men några av konsekvenserna av detta är ju bara löjeväckande och det var detta jag nämnde. Jag hade kunnat länka till andra källor och fått samma svar. Det finns ingen tydlig trend som säger att orkanerna ökar, varken i antal eller intensitet.
. Jag förnekar inte att temperaturen stiger och koldioxiden mycket väl kan vara orsaken till det, men några av konsekvenserna av detta är ju bara löjeväckande och det var detta jag nämnde. Jag hade kunnat länka till andra källor och fått samma svar. Det finns ingen tydlig trend som säger att orkanerna ökar, varken i antal eller intensitet.Model Validation and UncertaintyDom skriver också:
«PIOMAS has been extensively validated through comparisons with observations from US-Navy submarines, oceanographic moorings, and satellites. In addition model runs were performed in which model parameters and assimilation procedures were altered. From these validation studies we arrive at conservative estimates of the uncertainty in the trend of ± 1.0 10³ km³/decade. The uncertainty of the monthly averaged ice volume anomaly is estimated as ±0.75 10³ km³. Total volume uncertainties are larger than those for the anomaly because model biases are removed when calculating the anomalies. The uncertainty for October total ice volume is estimated to be ±1.35 10³ km³ . Comparison of winter total volumes with other volume estimates need to account for the fact that the PIOMAS domain currently does not extend southward far enough to cover all areas that can have winter time ice cover. Areas in the Sea of Okhotsk and in the Gulf of St. Lawrence are partially excluded from the domain. Details on model validation can be found in Schweiger et al. 2011 and (here). Additional information on PIOMAS can be found (here)
A comprehensive library of sea ice thickness data for model validation has been compiled and is available (here)»
http://psc.apl.uw.edu/research/projects/arctic-sea-ice-volume-anomaly/
‹Observations from satellites, Navy submarines, moorings, and field measurements are all limited in space and time. The assimilation of observations into numerical models currently provides one way of estimating sea ice volume changes on a continuous basis over several decades. Comparisons of the model estimates of the ice thickness with observations help test our understanding of the processes represented in the model that are important for sea ice formation and melt.›Din hypotes förefaller vara att vara att data är meningslösa.
Model Validation and UncertaintyDom skriver också:
«PIOMAS has been extensively validated through comparisons with observations from US-Navy submarines, oceanographic moorings, and satellites. In addition model runs were performed in which model parameters and assimilation procedures were altered. From these validation studies we arrive at conservative estimates of the uncertainty in the trend of ± 1.0 10³ km³/decade. The uncertainty of the monthly averaged ice volume anomaly is estimated as ±0.75 10³ km³. Total volume uncertainties are larger than those for the anomaly because model biases are removed when calculating the anomalies. The uncertainty for October total ice volume is estimated to be ±1.35 10³ km³ . Comparison of winter total volumes with other volume estimates need to account for the fact that the PIOMAS domain currently does not extend southward far enough to cover all areas that can have winter time ice cover. Areas in the Sea of Okhotsk and in the Gulf of St. Lawrence are partially excluded from the domain. Details on model validation can be found in Schweiger et al. 2011 and (here). Additional information on PIOMAS can be found (here)
A comprehensive library of sea ice thickness data for model validation has been compiled and is available (here)»
http://psc.apl.uw.edu/research/projects/arctic-sea-ice-volume-anomaly/
‹Observations from satellites, Navy submarines, moorings, and field measurements are all limited in space and time. The assimilation of observations into numerical models currently provides one way of estimating sea ice volume changes on a continuous basis over several decades. Comparisons of the model estimates of the ice thickness with observations help test our understanding of the processes represented in the model that are important for sea ice formation and melt.›Din hypotes förefaller vara att vara att data är meningslösa.
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