Bibliographic citations
Alvarez, E., (2024). Proyecciones climáticas de temperatura superficial del mar y nivel del mar en las costas de sudamérica y océano pacífico tropical usando modelos del CMIP5 [Universidad Nacional Agraria La Molina]. https://hdl.handle.net/20.500.12996/6540
Alvarez, E., Proyecciones climáticas de temperatura superficial del mar y nivel del mar en las costas de sudamérica y océano pacífico tropical usando modelos del CMIP5 []. PE: Universidad Nacional Agraria La Molina; 2024. https://hdl.handle.net/20.500.12996/6540
@misc{renati/243748,
title = "Proyecciones climáticas de temperatura superficial del mar y nivel del mar en las costas de sudamérica y océano pacífico tropical usando modelos del CMIP5",
author = "Alvarez Sanchez, Erick Alexis",
publisher = "Universidad Nacional Agraria La Molina",
year = "2024"
}
This Professional Proficiency Work (TSP) describes the obtaining of future scenarios for Sea Surface Temperature (SST) and Sea Level (NDM) using CMIP5 models, which was carried out within the framework of a consultancy at the National Service of Meteorology and Hydrology of Peru (SENAMHI). 16 models were analyzed, of which differences, trends and interrelationships were evaluated for the SST and NDM variables throughout the 21st century and historical period (1981-2005). For the differences, the average future period of: 2036-2065 and 2080-2100 was demonstrated. Thus, SST changes are obtained in the study sectors (in the Eastern Pacific) that range between 1°C - 2°C for the first period (2036-2065) and 2°C-4°C for the second (2080-2100) being the El Niño1+2 region where the greatest warming occurs. In the case of Sea Level, there are positive changes of 10 to 20 cm for 2036 2065 and changes between 20 - 40 cm (with some exceptions) for 2080-2100; adding that the IPSL-CMI5A-LR model is the only one that shows negative changes for our study sectors. On the other hand, in the global change in mean sea level we have a significant linear trend of 2.55 cm/decade for the CMIP5 models in the period 1981-2100. Finally, in the analysis of El Niño and La Niña events for the period 2071-2100, we obtain an increase in these episodes in 62.5% of the models.
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