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Article

Future Climate Projections for Tacna, Peru: Assessing Changes in Temperature and Precipitation

by
Gustavo De la Cruz
1,*,
Adrian Huerta
2,3,
Pablo Franco-León
4,
Edwin Pino-Vargas
5,
Lía Ramos-Fernández
6 and
Waldo Lavado-Casimiro
7
1
Doctoral Programme in Environmental Engineering and Science, La Molina National Agrarian University, Lima 15024, Peru
2
Institute of Geography, University of Bern, 3012 Bern, Switzerland
3
Oeschger Centre for Climate Change Research, University of Bern, 3012 Bern, Switzerland
4
Laboratory of Ecological Processes, Research Group of Arid Zones, Deserts and Climate Change (ADERIZA), Jorge Basadre Grohmann National University, Tacna 23000, Peru
5
Department of Civil Engineering, Jorge Basadre Grohmann National University, Tacna 23000, Peru
6
Department of Water Resources, La Molina National Agrarian University, Lima 15024, Peru
7
Directorate of Hydrology, National Meteorological and Hydrological Service of Peru (SENAMHI), Lima 15072, Peru
*
Author to whom correspondence should be addressed.
Atmosphere 2025, 16(2), 144; https://doi.org/10.3390/atmos16020144
Submission received: 28 November 2024 / Revised: 11 January 2025 / Accepted: 13 January 2025 / Published: 29 January 2025

Abstract

The Tacna region, situated in southwestern Peru, is distinguished by its desert and Andean zones, resulting in significant climatic variability. However, changes in future precipitation and temperature patterns could significantly impact sectors such as agriculture, energy, and water resources. In this context, this research analyzes climate scenarios of precipitation, maximum temperature (Tmax), and minimum temperature (Tmin) in Tacna. For this purpose, Tacna was divided into four homogeneous regions (Coast, Low Highlands, High Andes, and Andean Plateau) to assess future changes using CMIP6 climate models for the SSP1-2.6, SSP2-4.5, and SSP5-8.5 scenarios. A bias correction of these models was applied using the Quantile Delta Mapping method to improve accuracy. The validation results showed better performance for minimum temperature compared to maximum temperature and precipitation. Regarding the scenario results, by the end of the century, under the SSP5-8.5 scenario, Tmax could increase by up to +7 °C while Tmin could rise by up to +5 °C, particularly in the Andean Plateau. Precipitation is projected to decrease by up to 20% annually in higher elevations, albeit with considerable uncertainty; however, no significant changes are expected in seasonal patterns. This study underscores the importance of robust climate projections in formulating adaptation strategies for water resource management and infrastructure planning. The findings provide essential insights for decision-makers to address the challenges posed by climate change in vulnerable regions of southern Peru.
Keywords: Tacna; climate scenarios; precipitation; temperature Tacna; climate scenarios; precipitation; temperature

Share and Cite

MDPI and ACS Style

De la Cruz, G.; Huerta, A.; Franco-León, P.; Pino-Vargas, E.; Ramos-Fernández, L.; Lavado-Casimiro, W. Future Climate Projections for Tacna, Peru: Assessing Changes in Temperature and Precipitation. Atmosphere 2025, 16, 144. https://doi.org/10.3390/atmos16020144

AMA Style

De la Cruz G, Huerta A, Franco-León P, Pino-Vargas E, Ramos-Fernández L, Lavado-Casimiro W. Future Climate Projections for Tacna, Peru: Assessing Changes in Temperature and Precipitation. Atmosphere. 2025; 16(2):144. https://doi.org/10.3390/atmos16020144

Chicago/Turabian Style

De la Cruz, Gustavo, Adrian Huerta, Pablo Franco-León, Edwin Pino-Vargas, Lía Ramos-Fernández, and Waldo Lavado-Casimiro. 2025. "Future Climate Projections for Tacna, Peru: Assessing Changes in Temperature and Precipitation" Atmosphere 16, no. 2: 144. https://doi.org/10.3390/atmos16020144

APA Style

De la Cruz, G., Huerta, A., Franco-León, P., Pino-Vargas, E., Ramos-Fernández, L., & Lavado-Casimiro, W. (2025). Future Climate Projections for Tacna, Peru: Assessing Changes in Temperature and Precipitation. Atmosphere, 16(2), 144. https://doi.org/10.3390/atmos16020144

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