{"id":136,"date":"2023-02-01T08:39:34","date_gmt":"2023-02-01T08:39:34","guid":{"rendered":"https:\/\/workshops.issibern.ch\/tipmip\/?page_id=136"},"modified":"2025-08-21T12:51:49","modified_gmt":"2025-08-21T12:51:49","slug":"outreach-workshop-report","status":"publish","type":"page","link":"https:\/\/workshops.issibern.ch\/tipmip\/outreach-workshop-report\/","title":{"rendered":"Outreach (Workshop Report)"},"content":{"rendered":"
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Workshop Report\u00a0Tipping Points and Understanding EO data needs for a Tipping Element Model Intercomparison Project (TipMIP)<\/a>\u00a0by Annett Bartsch,\u00a0Hannah Liddy,\u00a0Mike Rast,\u00a0Narelle van der Wel,\u00a0Richard Wood, Sophie Hebden, Tim Lenton, Victor Brovkin<\/em><\/p>\n

It\u2019s fair to say that climate tipping points \u2014 defined by the Intergovernmental Panel on Climate Change (IPCC) as critical thresholds in a system that, when exceeded, can lead to a significant change in the state of the system \u2014 are by now a familiar concept, often used to convey the urgency of addressing climate change. World leaders at the COP27 climate conference of the UNFCCC in Sharm el-Sheik in November 2023 agreed on the need<\/a> to understand the impact of tipping points on the cryosphere.<\/p>\n

The growing popularity of this concept for motivating climate action also underscores the need for the scientific community to better understand the risks posed by self-reinforcing and difficult-to reverse processes taking place in the climate system. We need to understand the impacts that tipping points will have at different levels of global warming in order to guide mitigation and adaptation efforts.<\/p>\n

The risks gaining particular attention include shifts in the Amazon from rainforest to savannah, a slowing- and potential shutting down of the Atlantic Meridional Overturning Circulation (AMOC), ice loss from the Greenland and Antarctic ice sheets as well as growing CO2 and CH4 emissions from thawing permafrost. Our best global climate models don\u2019t yet include all potential climate tipping processes. This limits the scientific information available to guide policies to manage the risks to social systems, and we are still a long way from implementing an observing system that can monitor the onset of tipping points.<\/p>\n

Future Earth has been working closely with the World Climate Research Program (WCRP)<\/a> through the Earth Commission<\/a> and the AIMES global research network<\/a> to build the research agenda in this area, hosting a series of webinars focused on different climate tipping elements. One key research activity is to improve climate model representation of tipping elements through a model intercomparison exercise. From the observations side, researchers came together with climate modelers at a Workshop hosted at the International Space Science Institute<\/a> in Bern, Switzerland in October 2022, supported by the European Space Agency (ESA)-Future Earth joint program<\/a>.<\/p>\n

Animated discussions covered how Earth Observation (EO) together with modeling efforts can support monitoring and process understanding of tipping points and their interactions, climate feedbacks, and abrupt climate change more broadly. The EO and modeling communities have operated somewhat in silos. This workshop illustrated how important it is to get scientists from both communities into one room to understand one another\u2019s challenges and priorities. This is what was achieved in the ISSI Bern Workshop, and it highlighted how exciting it is to examine research questions from observational, modeling and theoretical perspectives.<\/p>\n

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What is TIPMIP?<\/h3>\n

Coordinated coupled-model intercomparison projects are a useful approach to assess our understanding of climate processes by providing a standard set of experiments and initialization data that can be run by individual climate modeling centers around the world. The differences in the model outputs create an ensemble of simulated climate behavior that can be used to explore the robustness or uncertainty \u2013 both spatially and temporally \u2013 of the processes involved.<\/p>\n

The \u2018TIPMIP\u2019 \u2013 TIPping element Model Intercomparison Project initiative, led by Earth Commissioner Ricarda Winkelmann, who is based at the Potsdam Institute for Climate Impact Research, will outline a set of experiments to explore the sensitivity of tipping behavior in response to rising levels of carbon dioxide in the atmosphere.<\/p>\n

There is not a strong quantitative understanding within the climate research community about the drivers or processes involved in triggering climate tipping points, since they often fall into the category of \u2018High Impact, but Low Likelihood\u2019 events, and so are seen fairly infrequently in model results. Therefore, the first phase of TIPMIP experiments will take a highly idealized approach that can be easily run by a range of models.<\/p>\n

It will begin with a set of experiments that provide a strong forcing of the climate system, with an increase in atmospheric CO2 of 1% per year. In addition, three more experiments will be defined to assess the impacts associated with specific levels of CO2. These experiments will lay the groundwork for understanding climate tipping behaviour and how societal activity can both drive and be impacted by abrupt change.<\/p>\n

Earth Observations for Direct Monitoring of Tipping Behavior<\/h3>\n

The limited temporal extent of the satellite record \u2013 spanning 4-5 decades at best \u2013 means that direct monitoring of trends and indicators for the onset of tipping points is restricted to \u2018fast\u2019 tipping points that occur over decades, that would apply to winter sea ice in the Arctic, the subpolar gyre, the Sahel\/Monsoon system, forest dieback \u2013 both tropical and boreal, freshwater ecosystems, and Arctic permafrost. The workshop heard of the potential to develop proxy indicators of tipping behavior and instabilities, for example to indicate the triggering of collapse of the Antarctic Ice Sheet.<\/p>\n

A major strength of EO is the ability to capture multiple temporal and spatial scales of tipping behavior, from local to regional to global, and from daily to interannual. Across these scales, there is potential for studying feedbacks in the Earth system that can lead to tipping points. There is opportunity to exploit satellite observations of the timing of events, to study extreme events and their impacts \u2013 including impacts on society, as well as cascading impacts and pace of change. The workshop identified the value of indicators with multiple variables that combine information from different sources to build a fuller picture of the processes occurring; for example to study the pressures affecting vegetation. It also called for better integration of EO data and platforms to facilitate the detection of tipping events.<\/p>\n

Earth Observation for Modeling<\/h3>\n

EO has a key role to play in improving the ability of climate models to project possible climate futures. Climate models rely on long-term EO datasets like the Essential Climate Variables (ECVs), many of which are based on remote sensing data. ECVs developed by programs like the ESA Climate Change Initiative<\/a> are used for model development, to assess model skill, (judged by how well models can reproduce past observations) and to constrain models \u2013 helping to determine certain parameters, for example, and to set initial conditions of part of the climate system at the start of a model simulation. The Global Climate Observing System (GCOS) is an international scientific body that maintains the definitions of the ECVs required for systematic observations of the Earth\u2019s climate. The goal is to help solve research challenges like climate tipping points, and to underpin climate services and adaptation measures.<\/p>\n

Applied to tipping points, there is huge scope to \u2018assimilate\u2019 \u2014 a statistical approach that brings the model\u2019s outputs closer to the observational data \u2014 EO to improve process-based models. For example, ocean color and sea surface temperature data could be used to better constrain biogeochemical or ecosystem processes in ocean ecosystem models to lower the uncertainty of predictions of thresholds and timescales of regime shifts.<\/p>\n

Research Frontiers<\/h3>\n

Recent wildfire and flooding events have highlighted society\u2019s fragility in the face of worsening climate extremes. Society also faces compound climate extremes whereby multiple hazards occur in the same location, or concurrent extremes occur at different locations. An open question is how extreme events might interplay with tipping points to drive worse impacts on society. Research frontiers will push our current EO datasets and modeling tools into new territory, in combinations that enable an exploration of the interactions between tipping points in the climate and society.<\/p>\n

Through this workshop and other coordinated efforts by Future Earth and WCRP, there will be more opportunities to engage with the tipping point research community and TIPMIP initiative. Recordings of past webinars and information about those upcoming can be accessed here<\/a>. Moreover, scientific sessions and meetings at EGU in April 2023 will be another opportunity for building bridges across scientific communities to enable us to better characterize the interfaces and identify and constrain the risks posed by tipping points.<\/p>\n

This report was orginally published on www.futureearth.org<\/a><\/em><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

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Workshop Report\u00a0Tipping Points and Understanding EO data needs for a Tipping Element Model Intercomparison Project (TipMIP)\u00a0by Annett Bartsch,\u00a0Hannah Liddy,\u00a0Mike Rast,\u00a0Narelle van der Wel,\u00a0Richard Wood, Sophie Hebden, Tim Lenton, Victor Brovkin It\u2019s fair to say that climate tipping points \u2014 defined by the Intergovernmental Panel on Climate Change (IPCC) as critical thresholds in a system that, […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-136","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/pages\/136","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/comments?post=136"}],"version-history":[{"count":2,"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/pages\/136\/revisions"}],"predecessor-version":[{"id":142,"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/pages\/136\/revisions\/142"}],"wp:attachment":[{"href":"https:\/\/workshops.issibern.ch\/tipmip\/wp-json\/wp\/v2\/media?parent=136"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}