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Characteristics of the low‐level jets observed over Dunkerque (North Sea French coast) using 4 years of wind lidar data
3.4.1 Land–sea thermal contrast Figure 9 presents the general distribution of the temperature difference between land and sea in the Dunkerque region, as defined in Section 2.3. This distribution is skewed toward negative values, meaning that the air over the southern Flanders Plain is more often colder than the air over the southern North Sea, with most values comprised between −4 K and +3 K.
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