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Skeptical Science New Research for Week #36, 2019

Posted on 10 September 2019 by Doug Bostrom

87 items this week, with 23 available as open access.

weekly-research

What are we doing on Mars?

We're from Earth, yet Included in this week's trawl of research articles are Streeter et al with Surface warming during the 2018/Mars Year 34 Global Dust Storm. Why are we visiting Mars today? Because the same storm that silenced the doughty Opportunity rover after over 14 years of operation yields an interesting research result on the dust-up's temporary effect on the Martian climate:

The impact of Mars’ 2018 Global Dust Storm (GDS) on surface and near?surface air temperatures was investigated using an assimilation of Mars Climate Sounder (MCS) observations. Rather than simply resulting in cooling everywhere from solar absorption (average surface radiative flux fell 26 Wm?2), the globally?averaged result was a 0.9 K surface warming. These diurnally?averaged surface temperature changes had a novel, highly non?uniform spatial structure, with up to 16 K cooling/19 K warming. Net warming occurred in low thermal inertia (TI) regions, where rapid night?time radiative cooling was compensated by increased longwave emission and scattering. This caused strong nightside warming, outweighing dayside cooling. The reduced surface?air temperature gradient closely coupled surface and air temperatures, even causing local dayside air warming. 

Note the similar causal mechanism and ultimate effect of increased surface temperatures to what a little additional CO2 in Earth's atmosphere produces. Despite a drastic reduction of surface energy delivery to Mars, night time temperatures rose and this effect was even true to some extent in day time.

Leaving aside dust not being gaseous, the principle and concerning difference between the two is that dust rapidly drops out of the atmosphere whether on Mars or at home, while the additional CO2 we've liberated into our local thin skin of gas will require several hundred years to find a permanent new home away from where it causes deleterious effects on our climate.

Lost in thought

It's continually surprising to see the almost laconic back-and-forth exploration of abstract economic matters as they apply to climate change, which to some of us seems to lack a sense of urgency or connection to the real world. Not to pick on them but simply as they appeared in this week's haul, as an example Mallapragada & Mignone bring us A theoretical basis for the equivalence between physical and economic climate metrics and implications for the choice of Global Warming Potential time horizon

The global warming potential (GWP) is widely used in policy analysis, national greenhouse gas (GHG) accounting, and technology life cycle assessment (LCA) to compare the impact of non-CO2 GHG emissions to the impact of CO2 emissions. While the GWP is simple and versatile, different views about the appropriate choice of time horizon—and the factors that affect that choice—can impede decision-making. If the GWP is viewed as an approximation to a climate metric that more directly measures economic impact—the global damage potential (GDP)—then the time horizon may be viewed as a proxy for the discount rate. However, the validity of this equivalence rests on the theoretical basis used to equate the two metrics. In this paper, we develop a new theoretical basis for relating the GWP time horizon and the economic discount rate that avoids the most restrictive assumptions of prior studies, such as an assumed linear relationship between economic damages and temperature. We validate this approach with an extensive set of numerical experiments using an up-to-date climate emulator that represents state-dependent climate-carbon cycle feedbacks. The numerical results largely confirm the theoretical finding that, under certain reasonable assumptions, time horizons in the GWP of 100 years and 20 years are most consistent with discount rates of approximately 3% and 7% (or greater), respectively.

Introduction of the "discount rate" into thinking about climate change mitigation and adaptation costs and expenditures confuses simple and ignorant minds (such as the author of this blog entry). Application of a scrupulously calculated discount rate to the question of spending related to climate change is promised to yield a brighter future.To this layperson establishing this magic number appears to be a form of paralytic perfectionism and as well seems dependent on unreliable information about a future beyond our ken. 

As a person who spends time on boats and yet fully intends to never fall overboard, I can spend a lot or a little on a "PFD" (personal flotation device) despite knowing full well that any such expenditure large or small will be much more productively employed in a true investment even at a very poor interest rate, per the advice of economic experts. The wisdom and promised benefits of not buying a PFD hold  true until the exact moment when I pitch overboard into cold water and shortly am depending on the PFD for continued survival, at which point more riches in the future become crisply abstract. Surely if I'm dead I won't be able to grow my personal economy; staying alive appears to be a prime requirement for my successful economic outcome. Thus I choose to waste money now on a quality PFD despite it not being a rational choice in the formal economic sense.

Assuming we'll stay high and dry may drive the decision to not buy a PFD and instead invest elsewhere. Similarly, overweening fascination with and pursuit of establishing theoretically defensible discount rates in connection with climate change appears to hinge on a relatively static scenario of a functioning economy resembling to some degree what we've come to expect from the past: a machine producing more or less steady and uninterrupted growth. It seems arguable that assumptions required to model such an economy and produce an academically worthy and admirable result are not necessarily valid given the broadly agreed dire projections we face of global warming and its various knock-on disruptions; we're entering an era with challenges on a scale and breadth we've not yet encountered and so old rules may not apply.

 What am I missing?  

Ideally an actual economist would explain this in terms an ordinary layperson might understand. Coming up for air and offering some conclusions with clear directions based on the assumption we will be falling overboard and indeed have already lost our grip and footing— are clumsily plunging over the lifelines into a life-threatening circumstance— would be very helpful. Is there an argument for obtaining a PFD, the notionally irrational choice to spend money to buy some better luck, a wager to help assure a future?

Articles:

Observation of climate warming

Influence of instrumentation on long temperature time series

Key Uncertainties in the Recent Air?Sea Flux of CO2

Linking Global Changes of Snowfall and Wet-bulb Temperature

Gap filling of monthly temperature data and its effect on climatic variability and trends

How accurate are modern climate reanalyses for the data-sparse Tibetan Plateau region?

Analysis of total column CO2 and CH4 measurements in Berlin with WRF-GHG (open access)

Impact of warming shelf waters on ice mélange and terminus retreat at a large SE Greenland glacier (open access)

Strong changes in englacial temperatures despite insignificantchanges in ice thickness at Dôme du Goûter glacier (Mont-Blanc area) (open access)

A long-term dataset of climatic mass balance, snow conditions, and runoff in Svalbard (1957–2018) (open access)

Is deoxygenation detectable before warming in the thermocline? (open access)

Half a century of satellite remote sensing of sea-surface temperature

Remote sensing of glacier and ice sheet grounding lines: A review

Analyses of observed features and future trend of extreme temperature events in Inner Mongolia of China

Chaotic signature of climate extremes

Characteristics of observed rainfall over Odisha: An extreme vulnerable zone in the east coast of India

HadUK?Grid—A new UK dataset of gridded climate observations (open access)

Physical science of global warming

Revised estimates of paleoclimate sensitivity over the past 800,000 years

Indian Ocean Warming Trend Reduces Pacific Warming Response to Anthropogenic Greenhouse Gases: An Interbasin Thermostat Mechanism

Ocean heat transport into the Barents Sea: Distinct controls on the upward trend and interannual variability

Warm Events Induce Loss of Resilience in Organic Carbon Production in the Northeast Pacific Ocean

Surface warming during the 2018/Mars Year 34 Global Dust Storm

Dynamics and thermodynamics of the mean Transpolar Drift and ice thickness in the Arctic Ocean

Brief communication: A submarine wall protecting the Amundsen Sea intensifies melting of neighboring ice shelves (open access)

Changes in the sensitivity of tropical rainfall response to local sea surface temperature anomalies under global warming

A review of the major drivers of the terrestrial carbon uptake: model-based assessments, consensus, and uncertainties (open access)

A missing component of Arctic warming: black carbon from gas flaring (open access)

Proglacial freshwaters are significant and previously unrecognized sinks of atmospheric CO2 (open access)

Biology of the warming planet

Biogeochemical anomalies at two southern California Current System moorings during the 2014?16 Warm Anomaly?El Niño sequence

Influence of late Quaternary climate on the biogeography of Neotropical aquatic species as reflected by non-marine ostracodes (open access)

Projecting marine species range shifts from only temperature can mask climate vulnerability

Secondary forest fragments offer important carbon?biodiversity co?benefits

Climate warming alters subsoil but not topsoil carbon dynamics in alpine grassland

Multiple stressor effects on coral reef ecosystems

Role of suspension feeders in antarctic pelagic-benthic coupling: Trophic ecology and potential carbon sinks under climate change

Effects of long-term exposure to reduced pH conditions on the shell and survival of an intertidal gastropod

Microbial responses to warming enhance soil carbon loss following translocation across a tropical forest elevation gradient

Modeling the warming climate

Sahelian precipitation change induced by SST increase: the contrasting roles of regional and larger?scale drivers

Probing the Sources of Uncertainty in Transient Warming on Different Time?Scales

Nonlinear response of extreme precipitation to warming in CESM1

Projected changes in daily variability and seasonal cycle of near-surface air temperature over the globe during the 21st century

Reproducing Internal Variability with Few Ensemble Runs

A modeling and process-oriented study to investigate the projected change of ENSO-forced wintertime teleconnectivity in a warmer world

Re-examining the first climate models: Climate sensitivity of a modern radiative-convective equilibrium model

Enhanced climate change response of wintertime North Atlantic circulation, cyclonic activity and precipitation in a 25 km-resolution global atmospheric model

Intercomparison and improvement of two-stream shortwave radiative transfer schemes in Earth system models for a unified treatment of cryospheric surfaces (open access)

Modeling the response of Greenland outlet glaciers to global warming using a coupled flow line–plume model (open access)

Applicability and consequences of the integration of alternative models for CO2 transfer velocity into a process-based lake model (open access)

Remapping of Greenland ice sheet surface mass balance anomalies for large ensemble sea-level change projections (open access)

Projected changes in mid?high latitude Eurasian climate during boreal spring in a 1.5oC and 2oC warmer world

Climate projections for glacier change modelling over the Himalayas

Statistical downscaling to project extreme hourly precipitation over the UK

Projected changes in rainfall and temperature over the Philippines from multiple dynamical downscaling models

Humans deal with our warming the climate

Evaluating climate change adaptation pathways through capital assessment: five case studies of forest social-ecological systems in France

The impact of climate change and variability on coffee production: a systematic review

The impact of temperature on mortality across different climate zones

A theoretical basis for the equivalence between physical and economic climate metrics and implications for the choice of Global Warming Potential time horizon (open access)

Social preferences for distributive outcomes of climate policy

Macro-economic analysis of green growth policies: the role of finance and technical progress in Italian green growth

Linking scales and disciplines: an interdisciplinary cross-scale approach to supporting climate-relevant ecosystem management (open access)

Does it matter if you “believe” in climate change? Not for coastal home vulnerability

Temperature and production efficiency growth: empirical evidence

Yield implications of date and cultivar adaptation to wheat phenological shifts: a survey of farmers in Turkey

Planned retreat in Global South megacities: disentangling policy, practice, and environmental justice

Climate change, natural hazards, and relocation: insights from Nabukadra and Navuniivi villages in Fiji

The accuracy of German citizens’ confidence in their climate change knowledge

Gendered perceptions of climate variability, food insecurity, and adaptation practices in Nepal (open access)

The future of agriculture and food: Evaluating the holistic costs and benefits

Evaluating China's water security for food production: The role of rainfall and irrigation

Characterization of Extreme Wet?Bulb Temperature Events in Southern Pakistan

Neglecting the urban? Exploring rural-urban disparities in the climate change–conflict literature on Sub-Sahara Africa

Global adaptation governance: An emerging but contested domain

Indigenous perceptions of climate anomalies in Malaysian Borneo

Valuation of nature and nature’s contributions to people (open access)

Rules to goals: emergence of new governance strategies for sustainable development (open access)

Energy demand transitions and climate mitigation in low-income urban households in India (open access)

Harvesting big data from residential building energy performance certificates: retrofitting and climate change mitigation insights at a regional scale (open access)

Urbanization and CO 2 emissions in resource-exhausted cities: evidence from Xuzhou city, China

The global cropland footprint of Denmark's food supply 2000–2013

Potentials and opportunities for low carbon energy transition in Vietnam: A policy analysis

Analysis of carbon tax efficiency in energy industries of selected EU countries

Quantifying carbon for agricultural soil management: from the current status toward a global soil information system (open access)

Carbon capture induced changes in Deccan basalt: a mass?balance approach

Suggestions

Please let us know if you're aware of an article you think may be of interest for Skeptical Science research news, or if we've missed something that may be important. Send your input to Skeptical Science via our contact form.

The previous edition of Skeptical Science new research may be found here. 

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Comments

Comments 1 to 6:

  1. We cannot quantify the effects of climate change and all possible feedback loops and tipping points to unstable chaotic systems. The correct analogy (as the author points out) is not a discount rate that quantifies the damage, but an insurance policy, like fire insurance. You don't invest in insurance to discount the damage, you do it to mitigate and hedge the risk. That's why with airplanes and nuclear plants, you go for 100% safety — you don't discount the likely damages. Think Boeing 737.

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  2. I often wonder what have we got to lose? If we reduce our reliance on fossil fuel use,everyone and the environment will benefit..if we continue with fossil fuel use and catastrophic postive feedback loops develop with no way to stop them getting worse, why take that chance? The status quo has to change or were dooming ourselves along with our currently rapidly accelerating 6th extinction event. I think our species will survive but never again at todays advanced level..

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  3. "...our species will survive but never again at todays advanced level."

    In the developed world we sit at the apex of a very fragile pyramid, our tap-and-swipe Eloi indolence supported by a spindly web of free market optimization. Earlier this year a 13 minute unscheduled power outage in Japan caused multi-month stoppage of some 1/3 of the world's NAND flash memory production, this manufacturing being highly concentrated, lacking redudancy but also extremely sensitive to disruptions. 

    One way to pitch fossil fuel preservation to folks who can't or won't understand its other problems might be to pitch it as a robust and easily exploited backup energy source for the case of another "Carrington Event." Ideally combustion of fossil fuels would be an exceptional activity, reserved for cases of emergency need. 

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  4. Grid reliability with renewables is a non issue that can be easily resolved. More and more renewables will push the system to the limits, which means storage will be required, such as battery storage or pumped hydro, and if the economics of this are problematic at scale, nuclear power can provide some of the storage function by providing stable baseload at moderate cost (not that I'm much of a nuclear power fan, but its an option) or limited use of gas fired for emergency shortages like DC says. The point is we have options going forwards. 

    www.prescouter.com/2017/12/renewable-energy-nuclear-power/

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  5. doug_bostrom@3,

    In addition to pitching fossil fuels for emergency energy needs, I would add that lots of easy to access fossil fuels could be incredibly helpful in the future for humans to mitigate the harmful effects of a natural extreme cooling event.

    In fact, that could even be pitched to a religious person as part of God's plan, for humans to figure out how to use the fossil fuels to off-set or limit harsh natural climate changes. God's plan could have been for humans to figure out the natural climate cycles and find and figure out how to extract fossil fuels, and save them in the ground for such a future emergency use. Humanity may even be able to use them in the event of an asteroid striking the planet.

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  6. nigelj@4,

    And new developments based on existing knowledge can also help, like the use of radiative cooling to produce power at night, as reported in this Bob McDonald science blog post on CBC News "Generating light from darkness"

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