Mutual effects of chemical stratification, global warming, and internal motions in a deep lake
Lake Iseo is a 256-m deep basin where a permanent chemical stratification has been established, preventing deep mixing and trapping the larger part of the incoming phosphorous in the monimolimnion. In this contribution, I will discuss the interplay between this stratified condition and the inflow and wind-driven motions, based on field and numerical studies.
Contact Eletta Negretti for more information or to schedule a discussion with the seminar speaker.