Stergios Misios
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View article: ClimateHub: Seasonal to Decadal Predictions for National Renewable Energy Management
ClimateHub: Seasonal to Decadal Predictions for National Renewable Energy Management Open
View article: Supplementary material to "Solar cycle impacts on North Atlantic climate"
Supplementary material to "Solar cycle impacts on North Atlantic climate" Open
View article: Solar cycle impacts on North Atlantic climate
Solar cycle impacts on North Atlantic climate Open
The North Atlantic sector has been identified as a region where the 11-year solar cycle has small but non-negligible impacts on near-surface climate. Nonetheless, debate persists about the robustness of such impacts and the mechanisms that…
View article: Natural Aerosols, Gaseous Precursors and Their Impacts in Greece: A Review from the Remote Sensing Perspective
Natural Aerosols, Gaseous Precursors and Their Impacts in Greece: A Review from the Remote Sensing Perspective Open
The Mediterranean, and particularly its Eastern basin, is a crossroad of air masses advected from Europe, Asia and Africa. Anthropogenic emissions from its megacities meet over the Eastern Mediterranean, with natural emissions from the Sah…
View article: Circulation Responses in the Southern Eastern Mediterranean to Large Volcanic Eruptions: The Katmai Eruption
Circulation Responses in the Southern Eastern Mediterranean to Large Volcanic Eruptions: The Katmai Eruption Open
The Etesian winds characterize the summertime circulation in the Eastern Mediterranean. Etesians are modulated by the Indian summer monsoon (ISM), but their response to other external forcings is not understood. Here, we investigate the re…
View article: StratoFIRE: Modeling Wildfire Smoke in the Stratosphere
StratoFIRE: Modeling Wildfire Smoke in the Stratosphere Open
The most extreme manifestation of a fire–weather interaction is the formation of pyrocumulonimbus (pyroCb) thunderstorms, triggered by super-heated updrafts, which can eject smoke at altitudes exceeding 20 Km. In this study, we inves…
View article: A 16-Year Climatology of Polar Stratospheric Clouds Based on CALIPSO Measurements (2006–2021) and Relationship with the Stratospheric Temperatures
A 16-Year Climatology of Polar Stratospheric Clouds Based on CALIPSO Measurements (2006–2021) and Relationship with the Stratospheric Temperatures Open
A 16-year global climatology of polar stratospheric clouds (PSCs) for the period 2006–2021 is produced, using satellite data products from the CALIOP lidar. The original Level 2 data (at 5 km horizontal and 180 m vertical resolution,…
View article: Aeolus winds impact on volcanic ash early warning systems for aviation
Aeolus winds impact on volcanic ash early warning systems for aviation Open
View article: Aeolus impact on Volcanic Ash early warning systems for Aviation
Aeolus impact on Volcanic Ash early warning systems for Aviation Open
Forecasting volcanic ash atmospheric pathways is of utmost importance for aviation. Volcanic ash can interfere with aircraft navigational instruments and can damage engine parts. Early warning systems, activated after volcanic eruptions ca…
View article: Decline in the Mediterranean Etesian winds after large volcanic eruptions in the last millennium
Decline in the Mediterranean Etesian winds after large volcanic eruptions in the last millennium Open
The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian low pressure systems. Etesi…
View article: Measurements of PG during rain, hail, snow and lightning
Measurements of PG during rain, hail, snow and lightning Open
We present an analysis of the evolution of PG during the course of rain, hail and snow events at the Xanthi site, N. Greece. In particular, using data from eight rain events in 2021, four hail events in the period 2018-2021 and four snow e…
View article: Decline in Etesian winds after large volcanic eruptions in the last millennium
Decline in Etesian winds after large volcanic eruptions in the last millennium Open
The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian low-pressure systems. Etesi…
View article: Reply on RC1
Reply on RC1 Open
Abstract. The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian …
View article: Reply on RC2
Reply on RC2 Open
Abstract. The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian …
View article: Comment on wcd-2022-16
Comment on wcd-2022-16 Open
Abstract. The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian …
View article: Comment on wcd-2022-16
Comment on wcd-2022-16 Open
Abstract. The northerly Etesian winds are a stable summertime circulation system in the eastern Mediterranean, emerging from a steep pressure gradient between the central Europe and Balkans high-pressure and the Anatolian …
View article: Measurements of PG during rain, hail, snow and lightning
Measurements of PG during rain, hail, snow and lightning Open
<p>We present an analysis of the evolution of PG during the course of rain, hail and snow events at the Xanthi site, N. Greece. In particular, using data from eight rain events in 2021, four hail events in the period 2018-2021 and fo…
View article: Supplementary material to "Decline of Etesian winds after large volcanic eruptions in the last millennium"
Supplementary material to "Decline of Etesian winds after large volcanic eruptions in the last millennium" Open
Sup. Figure 1 Probability density functions of a) Northerly WSP and b) NED for CESM-LME, 20CR and L-days (only in panel b).PDFs are calculated for the full period of each dataset.Dash lines in panel a) denote the full period median WSP of …
View article: Decline of Etesian winds after large volcanic eruptions in the last millennium
Decline of Etesian winds after large volcanic eruptions in the last millennium Open
Etesian winds represent one of the most stable summer circulation regimes in the Eastern Mediterranean. The Indian Summer Monsoon (ISM) variability and tropical/extra-tropical teleconnections are influencing the Eastern Mediterranean, give…
View article: Similar patterns of tropical precipitation and circulation changes under solar and greenhouse gas forcing
Similar patterns of tropical precipitation and circulation changes under solar and greenhouse gas forcing Open
Theory and model evidence indicate a higher global hydrological sensitivity for the same amount of surface warming to solar as to greenhouse gas (GHG) forcing, but regional patterns are highly uncertain due to their dependence on circulati…
View article: Simulating effects of the 774 AD solar proton event on atmospheric electricity
Simulating effects of the 774 AD solar proton event on atmospheric electricity Open
<p>High energy cosmic rays of galactic and solar origin, natural radioactivity, lighting in thunderstorms and electrified shower clouds, produce ion clusters and charge the whole atmosphere causing a ubiquitous potential difference b…
View article: Cause-and-effect relations between cosmic rays, electric field, aerosols and clouds
Cause-and-effect relations between cosmic rays, electric field, aerosols and clouds Open
<p>Here we examine the cause-and-effect relations between galactic cosmic rays, electric field, aerosols and clouds over a region of Atlantic Ocean, during a Forbush Decrease (FD) event on 07/12/2015, using Convergent Cross Mapping (…
View article: 4.2 `Top-down' versus `bottom-up' mechanisms for solar-climate coupling
4.2 `Top-down' versus `bottom-up' mechanisms for solar-climate coupling Open
View article: Historical Simulations With HadGEM3‐GC3.1 for CMIP6
Historical Simulations With HadGEM3‐GC3.1 for CMIP6 Open
We describe and evaluate historical simulations which use the third Hadley Centre Global Environment Model in the Global Coupled configuration 3.1 (HadGEM3‐GC3.1) and which form part of the UK's contribution to the sixth Coupled Model Inte…
View article: Etesian winds after major volcanic eruptions
Etesian winds after major volcanic eruptions Open
<p>Etesians winds are northerly winds in the lower atmosphere, blowing over the Aegean basin from early summer to early autumn, regulating summer time heating levels. The interannual variability of Etesians is thought to be linked to…
View article: Slowdown of the Walker circulation at solar cycle maximum
Slowdown of the Walker circulation at solar cycle maximum Open
The Pacific Walker Circulation (PWC) fluctuates on interannual and multidecadal timescales under the influence of internal variability and external forcings. Here, we provide observational evidence that the 11-y solar cycle (SC) affects th…
View article: A new observational solar spectral irradiance composite
A new observational solar spectral irradiance composite Open
International audience
View article: Update on Global Ozone: Past, Present, and Future, Chapter 3 in WMO Scientific Assessment of Ozone Depletion (2018)
Update on Global Ozone: Past, Present, and Future, Chapter 3 in WMO Scientific Assessment of Ozone Depletion (2018) Open
View article: Solar forcing for CMIP6 (v3.2)
Solar forcing for CMIP6 (v3.2) Open
This paper describes the recommended solar forcing dataset for CMIP6 and highlights changes with respect to CMIP5. The solar forcing is provided for radiative properties, namely total solar irradiance (TSI), solar spectral irradiance (SSI)…
View article: A new observational solar irradiance composite
A new observational solar irradiance composite Open
Variations in the solar spectral irradiance (SSI) are an important driver of the chemistry, temperature, and dynamics of the Earth's atmosphere and ultimately the Earth's climate. To investigate the detailed response of the Earth's atmosph…