Bachelorarbeit, 2017
43 Seiten, Note: 3,0
Geowissenschaften / Geographie - Meteorologie, Aeronomie, Klimatologie
1. Introduction
2. The representative Concentration Pathways
3. Origin of the data
4. Future periods 2021 – 2050 and 2071 - 2100
4.1 Winter mean temperatures
4.1.1 Warm and cold days
4.2 Extreme values of the maximum and minimum temperatures
4.3 Annual mean relative humidity
4.4 Annual mean precipitation
5. Reference period 1971 – 2000
5.1 Winter mean temperatures
5.1.1 Warm and cold days
5.2 Extreme values of the maximum and minimum temperatures
5.3 Annual mean relative humidity
5.4 Annual mean precipitation
6. Differences between reference and future periods
6.1 Differences in winter mean temperatures
6.1.1 Differences in warm and cold days
6.2 Differences of the extreme values
6.3 Differences in relative humidity
6.4 Differences in precipitation
7. Conclusion
This thesis aims to identify the expected changes in 2-meter temperature, daily precipitation, and relative humidity within the Mediterranean region (30°N–50°N, 10°W–45°E) under the RCP 2.6 scenario. By comparing future periods (2021–2050 and 2071–2100) against the reference period (1971–2000), the study evaluates whether the climate conditions of the Mediterranean area align with the 1.5°C global warming target set by the Paris Agreement.
1. Introduction
The following thesis focuses on the Mediterranean, in particular the region between the coordinates 30°N to 50°N and 10°W to 45°E. This work approaches the question “how the selected Representative Concentration Pathway (RCP) 2.6 W/m² values will be changing in the near (2021 - 2050) and far future (2071 - 2100) compared to the reference period (1971 – 2000)”. The Mediterranean area is characterized by mild and wet winters but also by hot and dry summers. Moreover, in the Mediterranean north the climate is arid and temperate whilst in its south it is rainy (Giorgi et al. 2008). Geographically, the Mediterranean area counts 21 countries (Sundseth, 2009) and lies between the subtropical and temperate climate zone (Bildungsserver, 2015). This supports the evaporation along with the decreasing of soil moisture and the flow of rivers. Such a development may produce a greater risk of future droughts and heatwaves (Bildungsserver, 2017). Very strong summers in the Mediterranean area are associated with Asian and African monsoons and a strong geopotential blocking (Giorgi et al. 2008). In the future, annual mean temperatures and annual precipitation over the entire European region will increase stronger than globally. It is projected that in Europe the largest warmings and the most increasing precipitation will occur in the Mediterranean area. In addition, the number of rainy days per year will mainly increase in the north.
Moreover, it is expected that there will be higher wind speed for the European region (IPCC, 2007). The motivation for this topic is that the Mediterranean area will be the most prominent hotspot for the climate change in the upcoming periods. An increase of aerosols in Central Europe, Africa and Asia will significantly influence the future climate of the Mediterranean area (Giorgi et al., 2008). Due to strongly decreasing precipitation in the central Mediterranean area in the recent years the soil moisture is massively affected.
1. Introduction: Defines the study area, the research question concerning climate changes in the Mediterranean, and highlights the region's vulnerability as a climate change hotspot.
2. The representative Concentration Pathways: Explains the RCP 2.6 "peak and decline" scenario, its relation to the Paris Agreement, and its unique characteristics compared to other RCP scenarios.
3. Origin of the data: Details the datasets utilized, specifically the CMIP5 and CORDEX projects, and describes the models (EC-Earth/RCA4) used for climate simulation.
4. Future periods 2021 – 2050 and 2071 - 2100: Provides a technical breakdown of the methodology and presents results for temperature, extreme values, humidity, and precipitation for the future periods.
5. Reference period 1971 – 2000: Establishes the baseline climate conditions for the Mediterranean region, using the same variables and metrics as the analysis for the future periods.
6. Differences between reference and future periods: Quantifies the climatic shifts by subtracting reference period data from future projection data, identifying significant differences in temperature, humidity, and precipitation.
7. Conclusion: Summarizes the key findings and concludes that the Mediterranean area under RCP 2.6 is likely to meet the first target of the Paris Agreement regarding global warming.
Mediterranean area, RCP 2.6, climate change, CMIP5, CORDEX, winter temperature, precipitation, relative humidity, global warming, Paris Agreement, EC-Earth, RCA4, radiative forcing, extreme values, climate modeling
The thesis investigates how climate variables—specifically 2-meter temperature, precipitation, and relative humidity—will change in the Mediterranean region under the RCP 2.6 climate scenario.
The central themes include the RCP 2.6 scenario characteristics, the methodology of regional climate modeling, and the specific projected environmental changes in the Mediterranean for the 21st century.
The main objective is to determine if the projected warming in the Mediterranean area under the RCP 2.6 conditions stays within the 1.5°C threshold defined by the Paris Agreement.
The study uses downscaled climate data from the CORDEX project, specifically the EC-Earth GCM and RCA4 RCM, to perform a comparative analysis between two future time horizons and a 1971–2000 reference period.
The main body examines the specific development of winter mean temperatures, extreme temperature events, relative humidity patterns, and annual precipitation trends for the periods 2021–2050 and 2071–2100.
Key terms include Mediterranean area, RCP 2.6, CMIP5, CORDEX, climate change, and various climate parameters like temperature, precipitation, and relative humidity.
It refers to the RCP 2.6 scenario, where radiative forcing increases until the mid-21st century and then decreases (declines) towards the end of the century.
The region is defined as the area lying between the coordinates 30°N to 50°N and 10°W to 45°E.
The 10-year run mean is used to smooth out annual variations and better recognize the long-term trends in temperature, humidity, and precipitation over the analyzed periods.
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