Show simple item record

dc.contributor.authorZhu, Y.
dc.contributor.authorAkiyoshi, H.
dc.contributor.authorAquila, V.
dc.contributor.authorAsher, E.
dc.contributor.authorBednarz, E.M.
dc.contributor.authorBekki, S.
dc.contributor.authorBrühl, C.
dc.contributor.authorButler, A.H.
dc.contributor.authorCase, P.
dc.contributor.authorChabrillat, S.
dc.contributor.authorChiodo, G.
dc.contributor.authorClyne, M.
dc.contributor.authorColarco, P.R.
dc.contributor.authorDhomse, S.
dc.contributor.authorFalletti, L.
dc.contributor.authorFleming, E.
dc.contributor.authorJohnson, B.
dc.contributor.authorJörimann, A.
dc.contributor.authorKovilakam, M.
dc.contributor.authorKoren, G.
dc.contributor.authorKuchar, A.
dc.contributor.authorLebas, N.
dc.contributor.authorLiang, Q.
dc.contributor.authorLiu, C.-C.
dc.contributor.authorMann, G.
dc.contributor.authorManyin, M.
dc.contributor.authorMarchand, M.
dc.contributor.authorMorgenstern, O.
dc.contributor.authorNewman, P.
dc.contributor.authorOman, L.D.
dc.contributor.authorØsterstrøm, F.F.
dc.contributor.authorPeng, Y.
dc.contributor.authorPlummer, D.
dc.contributor.authorQuaglia, I.
dc.contributor.authorRandel, W.
dc.contributor.authorRémy, S.
dc.contributor.authorSekiya, T.
dc.contributor.authorSteenrod, S.
dc.contributor.authorSukhodolov, T.
dc.contributor.authorTilmes, S.
dc.contributor.authorTsigaridis, K.
dc.contributor.authorUeyama, R.
dc.contributor.authorVisioni, D.
dc.contributor.authorWang, X.
dc.contributor.authorWatanabe, S.
dc.contributor.authorYamashita, Y.
dc.contributor.authorYu, P.
dc.contributor.authorYu, W.
dc.contributor.authorZhang, J.
dc.contributor.authorZhuo, Z.
dc.date2025
dc.date.accessioned2025-09-03T09:28:25Z
dc.date.available2025-09-03T09:28:25Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/14156
dc.descriptionThe 2022 Hunga volcanic eruption injected a significant amount of water vapor and a moderate amount of sulfur dioxide into the stratosphere, causing observable responses in the climate system. We have developed a model–observation comparison project to investigate the evolution of volcanic water and aerosols and their impacts on atmospheric dynamics, chemistry, and climate, using several state-of-the-art chemistry climate models. The project goals are (1) to evaluate the current chemistry–climate models to quantify their performance in comparison to observations and (2) to understand atmospheric responses in the Earth system after this exceptional event and investigate the potential impacts in the projected future. To achieve these goals, we designed specific experiments for direct comparisons to observations, for example from balloons and the Microwave Limb Sounder satellite instrument. Experiment 1 consists of two sets of free-running ensemble experiments from 2022 to 2031: one with fixed sea-surface temperatures and sea ice and one with coupled ocean. These experiments will help to understand the long-term evolution of water vapor and aerosols; quantify HTHH effects on stratospheric and mesospheric temperatures, dynamics, and transport; understand the impact of dynamic changes on ozone chemistry; quantify the net radiative forcings; and evaluate any surface climate impact. Experiment 2 is a nudged-run experiment from 2022 to 2023 using observed meteorology. To allow participation of more climate models with varying complexities of aerosol simulation, we include two sets of simulations in Experiment 2: Experiment 2a is designed for models with internally generated aerosol, while Experiment 2b is designed for models using prescribed aerosol surface area density. This experiment will help to analyze H2O and aerosol evolution, quantify the net radiative forcings, understand the impacts on mid-latitude and polar O3 chemistry, and allow close comparisons with observations.
dc.languageeng
dc.titleHunga Tonga–Hunga Ha′apai Volcano Impact Model Observation Comparison (HTHH-MOC) project: experiment protocol and model descriptions
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titleGeoscientific Model Development
dc.source.volume18
dc.source.issue17
dc.source.page5487-5512
Orfeo.peerreviewedYes
dc.identifier.doi10.5194/gmd-18-5487-2025
dc.identifier.url


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record