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UID:22550-1737450000-1761843600@www.iaa.csic.es
SUMMARY:Academic Spanish Course for Foreigners (2025)
DESCRIPTION:The Academic Spanish course for foreigners is designed to facilitate effective communication in academic and profesional contexts. Through a practical and personalized focus\, the participants will develop essential linguistic abilities to discuss scientific articles\, participate in conferences\, give presentations\, and collaborate in international projects. The program includes technical vocabulary\, beginner and advanced grammar\, and simulations of real-life situations. Moreover\, it will promote the cultural immersion to strengthen the comprehension of the Hispanic world\, and their impact on interdisciplinary investigation and collaboration. \nThis course will be taught throughout in the following blocks: \nJanuary 21st – February 27thApril 22nd – May 29thSeptember 23rd – October 30thThe course is taught by Prof. Nazira Ruíz
URL:https://www.iaa.csic.es/evento/academic-spanish-course-for-foreigners-2025/
LOCATION:IAA – CSIC\, Glorieta de la Astronomía\, Granada\, España
CATEGORIES:SO Training
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UID:25870-1751545800-1751549400@www.iaa.csic.es
SUMMARY:New clues about how Mars lost its water
DESCRIPTION:I will talk about a recent study led by IAA-CSIC focused on the atmospheric H escape during high obliquity period in recent Mars (average ~35º in last millions of years). Observations show that current thermal H escape (major water loss process) varies seasonally\, with considerable increases during dust storms of both  water abundance in the upper atmosphere and H escape rate. Present H-loss rates agree with 3D simulations by the Mars Planetary Climate Model used in this study\, varying with season between 1-11 x1026 atoms/s. However\, if we apply current escape rates to Mars’ entire history\, those values cannot fully explain the large volumes of ancient surface water suggested by several geological and mineralogical observatios. \nOur simulations with an obliquity of 35º indicate that the H escape rate could have been up to 20 times larger than today. The accumulated H loss over Mars history would translate into ~80 m Global Equivalent Layer\, aligning with the lower range of geological estimates and highlighting atmospheric H loss as a key factor in Mars’ desiccation. \nFecha: 03/07/2025 – 12:30Dr. Gabriella GilliIAA-CSIC \n 
URL:https://www.iaa.csic.es/evento/increased-hydrogen-escape-from-mars-atmosphere-during-periods-of-high-obliquity/
LOCATION:IAA – CSIC\, Glorieta de la Astronomía\, Granada\, España
CATEGORIES:Seminarios
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