Note for COP26 on Marine Cloud Brightening

2021 ◽  
Vol 6 (3) ◽  
Author(s):  
Salter SH ◽  

Present policies of most Governments, with a few predictable exceptions, concentrate on the desperate need to get to zero carbon emissions as soon as possible. This is a necessary but not sufficient objective. There is strong evidence from the Keeling curve in figure 1, about the difficulty (Figure 1). Figure 1: But if we could reduce, carbon emissions to zero the concentration of atmospheric greenhouse gases will be what we have now plus what we will be emitting between now and the zero-emission date minus the amount taken up by the oceans. This means that typhoons, floods, droughts, bushfires, sea-level rise, Arctic ice loss and damage to coral will all be worse, perhaps much worse than now. If you think that present conditions are not acceptable you have to conclude that zero is not low enough. As well as reducing emissions we will HAVE TO remove greenhouse gases, probably with help from phytoplankton, and also do direct cooling a soon as we can and hopefully ramp it down as emissions reduce [1].

2019 ◽  
pp. 7-22
Author(s):  
Gilbert E. Metcalf

Droughts, floods, soaring temperatures, sea-level rise, and melting ice are just some of the damages brought about by climate change. Chapter 1 details the cost of our failure to cut our emissions, from crop-destroying droughts to devastating floods. It also documents the inexorable build-up of greenhouse gases in the atmosphere as demonstrated by the Keeling curve and observations from Antarctic ice core samples. The chapter then provides a brief history of the science linking the build-up of atmospheric greenhouse gases and climate damages.


2015 ◽  
Vol 1 (8) ◽  
pp. e1500589 ◽  
Author(s):  
Ricarda Winkelmann ◽  
Anders Levermann ◽  
Andy Ridgwell ◽  
Ken Caldeira

The Antarctic Ice Sheet stores water equivalent to 58 m in global sea-level rise. We show in simulations using the Parallel Ice Sheet Model that burning the currently attainable fossil fuel resources is sufficient to eliminate the ice sheet. With cumulative fossil fuel emissions of 10,000 gigatonnes of carbon (GtC), Antarctica is projected to become almost ice-free with an average contribution to sea-level rise exceeding 3 m per century during the first millennium. Consistent with recent observations and simulations, the West Antarctic Ice Sheet becomes unstable with 600 to 800 GtC of additional carbon emissions. Beyond this additional carbon release, the destabilization of ice basins in both West and East Antarctica results in a threshold increase in global sea level. Unabated carbon emissions thus threaten the Antarctic Ice Sheet in its entirety with associated sea-level rise that far exceeds that of all other possible sources.


2020 ◽  
Author(s):  
Rosanne Martyr-Koller ◽  
Tabea Lissner ◽  
Carl-Friedrich Schleussner

<p>Climate impacts increase with higher warming and evidence is mounting that impacts increase strongly above 1.5°C. Therefore, adaptation needs also rise substantially at higher warming levels. Further<strong>, </strong>limits to adaptation will be reached above 1.5°C and loss and damage will be inferred. Coastal Nature-based Solutions (NbS) have arisen as popular adaptation options, particularly for coastal developing economies and Small Island Developing States (SIDS), because of their lower overall costs compared to traditional grey infrastructure approaches such as seawalls and levees; their economic co-benefits through positive effects on sectors such as tourism and fisheries; and a broader desire to shift toward so-called blue economies. Two NbS of particular interest for coastal protection are: 1) coral reefs, which reduce coastal erosion and flooding through wave attenuation; and 2) mangroves, which provide protection from storms, tsunamis and coastal erosion. Although there is international enthusiasm to implement these solutions, there is limited understanding of the future viability of these ecosystems, particularly in their capacities as coastal adaptation service providers, in a warmer world.</p><p>In this presentation, we highlight how long and with how much coverage coral and mangrove ecosystems can provide coastal protection services for future climate scenarios, using air temperature and sea level rise as climate change indicators. A mathematical model for each ecosystem is developed, based on the physical parameters necessary for the sustainability of these ecosystems. We investigate the protective capabilities of each ecosystem under warming and sea level rise scenarios compatible with: below 1.5°C warming; below 2°C warming; warming based on current global commitments to carbon emissions reductions (3-3.5°C); and with no carbon mitigation (6°C). Results show what temperature and sea level rise values beyond which these ecosystems can no longer provide coastal protective services. These results have also been framed in a temporal window to show when these services may not be feasible, beyond which more costly adaptation measures and/or loss and damage may be incurred.</p>


2012 ◽  
Vol 39 (19) ◽  
Author(s):  
Richard G. Williams ◽  
Philip Goodwin ◽  
Andy Ridgwell ◽  
Philip L. Woodworth

2012 ◽  
Vol 4 (3) ◽  
pp. 212-229 ◽  
Author(s):  
K. Kvale ◽  
K. Zickfeld ◽  
T. Bruckner ◽  
K. J. Meissner ◽  
K. Tanaka ◽  
...  

Abstract Anthropogenic emissions of greenhouse gases could lead to undesirable effects on oceans in coming centuries. Drawing on recommendations published by the German Advisory Council on Global Change, levels of unacceptable global marine change (so-called guardrails) are defined in terms of global mean temperature, sea level rise, and ocean acidification. A global-mean climate model [the Aggregated Carbon Cycle, Atmospheric Chemistry and Climate Model (ACC2)] is coupled with an economic module [taken from the Dynamic Integrated Climate–Economy Model (DICE)] to conduct a cost-effectiveness analysis to derive CO2 emission pathways that both minimize abatement costs and are compatible with these guardrails. Additionally, the “tolerable windows approach” is used to calculate a range of CO2 emissions paths that obey the guardrails as well as a restriction on mitigation rate. Prospects of meeting the global mean temperature change guardrail (2° and 0.2°C decade−1 relative to preindustrial) depend strongly on assumed values for climate sensitivity: at climate sensitivities >3°C the guardrail cannot be attained under any CO2 emissions reduction strategy without mitigation of non-CO2 greenhouse gases. The ocean acidification guardrail (0.2 unit pH decline relative to preindustrial) is less restrictive than the absolute temperature guardrail at climate sensitivities >2.5°C but becomes more constraining at lower climate sensitivities. The sea level rise and rate of rise guardrails (1 m and 5 cm decade−1) are substantially less stringent for ice sheet sensitivities derived in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report, but they may already be committed to violation if ice sheet sensitivities consistent with semiempirical sea level rise projections are assumed.


2016 ◽  
Vol 23 (1) ◽  
pp. 37-57 ◽  
Author(s):  
Joanna Wibig

Abstract This paper outlines the symptoms of contemporary global warming, reviews its possible driving factors and presents some projections for future. Key among the symptoms are those related to temperature, with the increase in average global temperature since 1880 now reaching a value of 0.85°C. While warming has encompassed almost the whole world, the high latitudes have warmed more than the low, and maximum temperature has increased more than average temperature. Warming has been causing sea level rise, thanks to both the thermal expansion of warming water and the melting of ice on land. The other consequence of warming is a change in precipitation pattern, manifesting itself in higher precipitation in certain parts of the world (generally at low and high latitudes), but also lower precipitation in other parts (mainly the Tropics); as well as in changes in the intraannual course characterising precipitation (with more falling in winter and less in summer), and in the frequency and intensity of rainfall (more intense heavy-precipitation events and higher variability where the frequency of precipitation is concerned). Among the possible driving factors, the most important are those related to the increase of CO2 and mixing ratios of other greenhouse gases in the troposphere. Land-use changes and emissions of aerosols to the atmosphere also exert a major impact on temperature. These are mainly anthropogenic factors. While natural drivers also modulate the climate markedly, they tend to warm and cool the globe alternately, stepping up warming when they are in a warming phase, but slowing down or even offsetting warming during a cooling phase. Projections for the future are entirely dependent on socio-economic scenarios of future development. All the (economically) realistic scenarios point to a continuation of the warming trend, with a further intense sea-level rise and precipitation changes, albeit with the rate of change varying in line with the rate of increase in concentrations of the greenhouse gases. The realistic range of values for average rise in global temperature is between 2 and even 6 degrees Celsius.


Author(s):  
Robert Mendelsohn

Emissions from greenhouse gases are predicted to cause climate to change. Increased solar radiation gradually warms the oceans, which leads to warmer climates. How much future climates will change depends on the cumulative emissions of greenhouse gases, which in turn depends on the magnitude of future economic growth. The global warming caused by humanmade emissions will likely affect many phenomena across the planet. The future damage from climate change is the net damage that these changes will cause to mankind. Oceans are expected to expand with warmer temperatures, and glaciers and ice sheets are expected to melt, leading to sea level rise over time (a damage). Crops tend to have a hill-shaped relationship with temperature, implying that some farms will be hurt by warming and some farms will gain, depending on their initial temperature. Cooling expenditures are expected to increase (a damage), whereas heating expenditures are expected to fall (a benefit). Water is likely to become scarcer as the demand for water increases with temperature (a damage). Warming is expected to cause ecosystems to migrate poleward. Carbon fertilization is expected to cause forest ecosystems to become more productive, but forest fires are expected to be more frequent so that it is uncertain whether forest biomass will increase or decrease. The expected net effect of all these forest changes is an increase in timber supply (a benefit). It is not known how ecosystem changes will alter overall enjoyment of ecosystems. Warmer summer temperatures will cause health effects from heat waves (a damage), but even larger reductions in health effects from winter cold (a benefit). Large tropical cyclones are expected to get stronger, which will cause more damage from floods and high winds. Winter recreation based on snow will be harmed, but summer outdoor recreation will enjoy a longer season, leading to a net benefit. The net effect of historic climate change over the last century has been beneficial. The beneficial effects of climate change have outweighed the harmful effects across the planet. However, the effects have not been evenly distributed across the planet, with more benefits in the mid to high latitudes and more damage in the low latitudes. The net effect of future climate is expected to turn harmful as benefits will shrink and damages will become more pervasive. A large proportion of the damage from climate change will happen in the low latitudes, where temperatures will be the highest. Measurements of the economic impact of climate change have changed over time. Early studies focused only on the harmful consequences of climate change. Including climate effects that are beneficial has reduced net damage. Early studies assumed no adaptation to climate change. Including adaptation has reduced the net harm from climate change. Catastrophe has been assumed to be a major motivation to do near-term mitigation. However, massive sea level rise, ecosystem collapse, and high climate sensitivity are all slow-moving phenomena that take many centuries to unfold, suggesting a modest present value.


2015 ◽  
Vol 112 (44) ◽  
pp. 13508-13513 ◽  
Author(s):  
Benjamin H. Strauss ◽  
Scott Kulp ◽  
Anders Levermann

Anthropogenic carbon emissions lock in long-term sea-level rise that greatly exceeds projections for this century, posing profound challenges for coastal development and cultural legacies. Analysis based on previously published relationships linking emissions to warming and warming to rise indicates that unabated carbon emissions up to the year 2100 would commit an eventual global sea-level rise of 4.3–9.9 m. Based on detailed topographic and population data, local high tide lines, and regional long-term sea-level commitment for different carbon emissions and ice sheet stability scenarios, we compute the current population living on endangered land at municipal, state, and national levels within the United States. For unabated climate change, we find that land that is home to more than 20 million people is implicated and is widely distributed among different states and coasts. The total area includes 1,185–1,825 municipalities where land that is home to more than half of the current population would be affected, among them at least 21 cities exceeding 100,000 residents. Under aggressive carbon cuts, more than half of these municipalities would avoid this commitment if the West Antarctic Ice Sheet remains stable. Similarly, more than half of the US population-weighted area under threat could be spared. We provide lists of implicated cities and state populations for different emissions scenarios and with and without a certain collapse of the West Antarctic Ice Sheet. Although past anthropogenic emissions already have caused sea-level commitment that will force coastal cities to adapt, future emissions will determine which areas we can continue to occupy or may have to abandon.


2021 ◽  
Vol 50 ◽  
pp. 245-259
Author(s):  
Rosanne Martyr-Koller ◽  
Adelle Thomas ◽  
Carl-Friedrich Schleussner ◽  
Alexander Nauels ◽  
Tabea Lissner

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