欢乐中国
发表于 2025-3-28 17:20:38
Dieter Nelles,Hartmut Opperskalskiultidecadal. Statistical analysis is playing an important role in advancing our knowledge of air-sea interaction and its influence on worldwide climate variability. So this chapter is particularly well-suited for illustrating an application of statistics in climatology.
Ballerina
发表于 2025-3-28 18:58:35
Arten des digitalen Storytellingsnd that this skill is known in advance by the user. Two “no-skill” forecast schemes would be random forecasts or constant (e.g. fixed climatology) forecasts. An additional factor relevant to a scheme’s usefulness is its efficiency — in other words its skill with respect to more simple forecast schemes (like persistence of existing conditions).
他日关税重重
发表于 2025-3-28 22:59:19
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defile
发表于 2025-3-29 06:15:33
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失望昨天
发表于 2025-3-29 07:38:01
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剥削
发表于 2025-3-29 14:14:54
Analysing the Boreal Summer Relationship Between Worldwide Sea-Surface Temperature and Atmospheric Vultidecadal. Statistical analysis is playing an important role in advancing our knowledge of air-sea interaction and its influence on worldwide climate variability. So this chapter is particularly well-suited for illustrating an application of statistics in climatology.
Ligament
发表于 2025-3-29 18:33:57
The Evaluation of Forecastsnd that this skill is known in advance by the user. Two “no-skill” forecast schemes would be random forecasts or constant (e.g. fixed climatology) forecasts. An additional factor relevant to a scheme’s usefulness is its efficiency — in other words its skill with respect to more simple forecast schemes (like persistence of existing conditions).
蔓藤图饰
发表于 2025-3-29 23:23:04
Spatial Patterns: EOFs and CCAe dynamics of the considered process. The “noise subspace”, on the other hand, is high-dimensional and contains all processes which are purportedly irrelevant in their details for the “signal subspace”.
防御
发表于 2025-3-30 01:21:13
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Visual-Acuity
发表于 2025-3-30 07:47:32
Ralf T. Kreutzer,Karl-Heinz Landistics of the atmospheric variables, the concept of the stochastic climate model is introduced in this chapter. Its application to climate variations is then illustrated in the context of the midlatitude sea surface temperature anomalies. The other applications are then briefly discussed.