Greece Climate Resilience Policy Indicator
This report is part of Climate Resilience Policy Indicator
Country summary
- Greece’s mean annual temperature has been increasing since the 1960s, and in the last two decades its rate of warming has accelerated to overtake the world average. Greece’s average annual temperature is projected to continue rising through the end of the century with seasonal and geographical variations. Higher annual mean temperatures and more frequent extreme heat events could threaten its electricity supply security.
- Most regions of Greece recorded negative rainfall trends in the second half of the 20th century. These trends are expected to continue throughout the 21st century and could be particularly accentuated in the summer. Less precipitation, combined with rising temperatures, could lead to lower thermal power and hydropower output.
- Greece’s National Adaptation Strategy includes the energy sector as one of its 15 priority areas for adaptation, and it proposes actions for climate resilience, such as installing smart networks for demand-side management; incorporating precautionary measures into energy infrastructure planning; and conducting vulnerability assessments for energy networks, plants and facilities. It also suggests measures to safeguard the existing energy system, protect water resources used for power generation and enable research and development of new technologies. Regional Adaptation Action Plans – which complement the National Adaptation Strategy by applying its goals to individual regional circumstances, priorities and needs – include dedicated climate change vulnerability and impact assessments to identify vulnerability hotspots, as well as actions for energy sector adaptation.
Climate hazard assessment
Temperature
Greece’s annual mean temperature has clearly been increasing: for 2001-2015, most meteorological stations reported mean annual temperatures were higher than for 1961-2000. In the past two decades, the average rate of warming was 0.047°C per year – 0.011°C above the world average.
By the end of the century, Greece’s mean air temperature is expected to be 3-4.5ºC higher than during the 1961-1990 reference period, with marked seasonal disparities. Under a high-emissions scenario, temperature increases in summer (+5.4°C) and autumn (+4.7°C) are projected to be higher than in spring (+3.9°C). Warming is expected to be more pronounced in continental regions than in the islands for all seasons except autumn, during which season the temperature rise is expected to be more uniform across the country.
According to Greece’s risk assessment report, higher temperatures are expected to present electricity supply risks. Warming can not only reduce the efficiency of thermal power plants but increase their need for cooling water. Rapid rises in peak electricity demand for cooling during extreme heat events may prompt failures, as happened in 2017 and 2021 when escalating power demand during heatwaves resulted in several power outages despite Public Power Corporation (PPC) preparation efforts.
Furthermore, sea level increases due to global warming are projected to continue throughout the 21st century, with the water level rising 0.2-2 metres by 2100. Greece’s coastal areas are home to most of the country’s socioeconomic activity as well as key energy infrastructure such as electricity transmission lines. As 21% of its total shoreline has a medium or high level of vulnerability to sea level rises, energy infrastructure in coastal areas could be adversely affected by shoreline retreat.
Temperature in Greece, 2000-2020
OpenPrecipitation
Most regions of Greece registered a negative rainfall trend over the course of the 20th century, with drops ranging from 10% in Eastern Greece to 20% in Western Greece. Climate projections show a further decrease in precipitation by the end of the 21st century, with higher-emissions scenarios demonstrating a more pronounced drop with stronger seasonal and geographical disparities. For example, there could be 17% less precipitation by the end of the century than during the reference period (1961-1990), with a risk of summer precipitation dropping by nearly half (-47%) under a high-emissions scenario.
The Northern Aegean region is expected to have the mildest decrease in precipitation, while the Eastern Peloponnese and all other regions are projected to experience a stronger decline. Less precipitation, combined with higher temperatures, is likely to reduce power generation output. According to Greece’s latest UNFCCC communication, this fall in electricity output may require the country to install additional generation capacity.
Tropical cyclones and storms
Although Greece is not exposed to tropical cyclones, storms challenge its energy sector, as exemplified by April 2019 storms that provoked power outages, first in central Athens and then in several suburbs of east Athens and Piraeus.1 Damage from high windspeeds can be compounded by heavy rains, such as during the September 2020 storm that hit Western Greece, causing power outages and flooding and affecting both energy supply and transport.
Policy readiness for climate resilience
Greece’s national climate policies clearly address energy sector climate resilience. The National Adaptation Strategy (NAS), developed by Greece’s Ministry of Environment and Energy and endorsed by its parliament in 2016, includes the energy sector as one of 15 target areas and offers a list of possible actions and measures. NAS formulation was based on stakeholder consultations and the national climate impact assessment published by the Climate Change Impacts Study Committee of the Bank of Greece in 2011.
This assessment highlights the risk of climate change impacts on seasonal patterns of energy demand and power supply networks, and based on this information the NAS proposes actions to strengthen energy’s sector climate resilience. It recommends installing smart networks for demand-side management; incorporating precautionary measures to avoid climate risks when planning energy infrastructure; and conducting vulnerability assessments of different types of energy networks, plants and facilities. It also suggests actions to safeguard the existing energy system (mainland, coastal and insular energy infrastructure), protect water resources used for power generation, and enable research and development of new technologies (including smart grids).
Thirteen Regional Adaptation Action Plans (RAAPs) complement NAS activities by applying NAS goals, principles and priorities – and potential sectoral adaptation measures – to particular regional circumstances, priorities and needs. The RAAPs include regional climate change impact assessments and tailored actions based on region-specific climate impacts and vulnerabilities. They also identify ways to adapt energy infrastructure to climate change and to smooth the peaks associated with higher energy demand for cooling in the housing and tourism sectors.
In 2017, the Ministry of Environment and Energy submitted a proposal to support NAS and RAAP implementation to the EU LIFE Programme, the European Union’s funding instrument for environmental and climate action. The LIFE-IP AdaptInGR project provides Greece with human and financial resources to help it implement adaptation actions by 2026, including those related to the energy sector.
Furthermore, to enable Greece to formulate and implement energy sector adaptation policies, the LIFE-IP AdaptInGR project is currently analysing the 13 RAAPs to identify necessary national-level actions. It also aims to assess current adaptation measures in energy legislation, strategies, plans and funding tools to identify progress, difficulties, knowledge gaps, strengths, opportunities and priorities for action.
Compared with the NAS, actions for climate resilience in the energy sector are less highlighted or rarely mentioned in national energy policies and laws such as the National Energy and Climate Plan, Law No. 3855/2010 on Measures to Improve Energy Efficiency in End Use, Energy Services and Other Provisions, and Law No. 4001/2011 on the Operation of Electricity and Gas Energy Markets for Exploration, Production and Transmission Networks of Hydrocarbons.
References
“Storms” refer to any disturbed state of the atmosphere, strongly implying destructive and unpleasant weather, and can range in scale. “Tropical cyclone” is the general term for a strong, cyclonic-scale disturbance that originates over tropical oceans. Although this report uses these terms generally, they can be divided into detailed categories: a tropical storm is a tropical cyclone with one-minute average surface winds of 18‑32 m/s. Beyond 32 m/s, a tropical cyclone is called a hurricane, typhoon or cyclone depending on its geographic location. Hurricanes refer to the high-intensity cyclones that form in the South Atlantic, central North Pacific and eastern North Pacific; typhoons occur in the northwest Pacific; and the more general term cyclone applies to the South Pacific and Indian oceans.
Reference 1
“Storms” refer to any disturbed state of the atmosphere, strongly implying destructive and unpleasant weather, and can range in scale. “Tropical cyclone” is the general term for a strong, cyclonic-scale disturbance that originates over tropical oceans. Although this report uses these terms generally, they can be divided into detailed categories: a tropical storm is a tropical cyclone with one-minute average surface winds of 18‑32 m/s. Beyond 32 m/s, a tropical cyclone is called a hurricane, typhoon or cyclone depending on its geographic location. Hurricanes refer to the high-intensity cyclones that form in the South Atlantic, central North Pacific and eastern North Pacific; typhoons occur in the northwest Pacific; and the more general term cyclone applies to the South Pacific and Indian oceans.