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Abstract The time water vapor spends in the atmosphere from evaporation to precipitation, termed here the water vapor lifetime, is of fundamental relevance for characterizing the water cycle, for the turnover of mass and energy, causes of precipitation extremes, and the recycling of precipitation over land. While the global average lifetime of water vapor is commonly considered as about 8β10 days, recent work indicates that the distribution of water vapor lifetimes is highly skewed, and that a large part of the water vapor could have average lifetimes of about 4β5 days. Besides calling for scrutiny of these new estimates, these findings also prompt an investigation of the factors shaping the distribution of the lifetime of water vapor. Using idealized setups and reanalysis data, I explore the influence of heterogeneity and nonstationarity on water vapor age and lifetime. The combination of nonstationarity and heterogeneity allows for short and long local lifetimes and water vapor ages, while maintaining tπ Venue: The Loud
π Address: 741 6th Ave
πΊοΈ Extended Address: Huntington, WV 25701
π City: Huntington
π Location: 38.4174, -82.4449Error occurred: DateTime::__construct(): Failed to parse time string (The Loud) at position 0 (T): The timezone could not be found in the database
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The Loud, 741 6th Ave, Huntington, WV 25701, US, United States
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