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OKIsItJustMe's Journal2018 Fourth Warmest Year in Continued Warming Trend, According to NASA, NOAA
(Please note, NASA press releaseCopyright concerns are nil.)
https://www.nasa.gov/press-release/2018-fourth-warmest-year-in-continued-warming-trend-according-to-nasa-noaa
RELEASE 19-002
2018 Fourth Warmest Year in Continued Warming Trend, According to NASA, NOAA
Earth's global surface temperatures in 2018 were the fourth warmest since 1880, according to independent analyses by NASA and the National Oceanic and Atmospheric Administration (NOAA).
Global temperatures in 2018 were 1.5 degrees Fahrenheit (0.83 degrees Celsius) warmer than the 1951 to 1980 mean, according to scientists at NASAs Goddard Institute for Space Studies (GISS) in New York. Globally, 2018's temperatures rank behind those of 2016, 2017 and 2015. The past five years are, collectively, the warmest years in the modern record.
2018 is yet again an extremely warm year on top of a long-term global warming trend, said GISS Director Gavin Schmidt.
Since the 1880s, the average global surface temperature has risen about 2 degrees Fahrenheit (1 degree Celsius). This warming has been driven in large part by increased emissions into the atmosphere of carbon dioxide and other greenhouse gases caused by human activities, according to Schmidt.
Earths long-term warming trend can be seen in this visualization of NASAs global temperature record, which shows how the planets temperatures are changing over time, compared to a baseline average from 1951 to 1980. The record is shown as a running five-year average.
Credits: NASAs Scientific Visualization Studio/Kathryn Mersmann
Download high-definition video and still imagery here.
Weather dynamics often affect regional temperatures, so not every region on Earth experienced similar amounts of warming. NOAA found the 2018 annual mean temperature for the contiguous 48 United States was the 14th warmest on record.
Warming trends are strongest in the Arctic region, where 2018 saw the continued loss of sea ice. In addition, mass loss from the Greenland and Antarctic ice sheets continued to contribute to sea level rise. Increasing temperatures can also contribute to longer fire seasons and some extreme weather events, according to Schmidt.
The impacts of long-term global warming are already being felt in coastal flooding, heat waves, intense precipitation and ecosystem change, said Schmidt.
NASAs temperature analyses incorporate surface temperature measurements from 6,300 weather stations, ship- and buoy-based observations of sea surface temperatures, and temperature measurements from Antarctic research stations.
This line plot shows yearly temperature anomalies from 1880 to 2018, with respect to the 1951-1980 mean, as recorded by NASA, NOAA, the Japan Meteorological Agency, the Berkeley Earth research group, and the Met Office Hadley Centre (UK). Though there are minor variations from year to year, all five temperature records show peaks and valleys in sync with each other. All show rapid warming in the past few decades, and all show the past decade has been the warmest.
Credits: NASAs Earth Observatory
These raw measurements are analyzed using an algorithm that considers the varied spacing of temperature stations around the globe and urban heat island effects that could skew the conclusions. These calculations produce the global average temperature deviations from the baseline period of 1951 to 1980.
Because weather station locations and measurement practices change over time, the interpretation of specific year-to-year global mean temperature differences has some uncertainties. Taking this into account, NASA estimates that 2018s global mean change is accurate to within 0.1 degree Fahrenheit, with a 95 percent certainty level.
NOAA scientists used much of the same raw temperature data, but with a different baseline period and different interpolation into the Earths polar and other data poor regions. NOAAs analysis found 2018 global temperatures were 1.42 degrees Fahrenheit (0.79 degrees Celsius) above the 20th century average.
NASAs full 2018 surface temperature data set and the complete methodology used to make the temperature calculation are available at:
https://data.giss.nasa.gov/gistemp
GISS is a laboratory within the Earth Sciences Division of NASAs Goddard Space Flight Center in Greenbelt, Maryland. The laboratory is affiliated with Columbia Universitys Earth Institute and School of Engineering and Applied Science in New York.
NASA uses the unique vantage point of space to better understand Earth as an interconnected system. The agency also uses airborne and ground-based monitoring, and develops new ways to observe and study Earth with long-term data records and computer analysis tools to better see how our planet is changing. NASA shares this knowledge with the global community and works with institutions in the United States and around the world that contribute to understanding and protecting our home planet.
For more information about NASAs Earth science missions, visit:
https://www.nasa.gov/earth
The slides for the Feb. 6 news conference are available at:
https://www.nasa.gov/sites/default/files/atoms/files/noaa-nasa_global_analysis-2018-final_feb6.pdf
NOAAs Global Report is available at:
http://bit.ly/Global201812
-end-
Steve Cole
Headquarters, Washington
202-358-0918
stephen.e.cole@nasa.gov
Last Updated: Feb. 6, 2019
Editor: Sean Potter
Diffusing the methane bomb: We can still make a difference
http://www.iiasa.ac.at/web/home/about/news/190206-Tundra-methane.htmlDiffusing the methane bomb: We can still make a difference
The Arctic is warming twice as fast as the rest of the planet, causing the carbon containing permafrost that has been frozen for tens or hundreds of thousands of years to thaw and release methane into the atmosphere, thereby contributing to global warming. The findings of a study that included researchers from IIASA, however, suggest that it is still possible to neutralize this threat
In their analysis, the researchers quantified the upper range value for natural methane emissions that can be released from the Arctic tundra, as it allows it to be put in relation to the much larger release of methane emissions from human activities. Although estimates of the release of methane from natural sources in the Arctic and estimates of methane from human activity have been presented separately in previous studies, this is the first time that the relative contribution of the two sources to global warming has been quantified and compared.
According to the researchers, their findings confirm the urgency of a transition away from a fossil fuel based society as well as the importance of reducing methane emissions from other sources, in particular livestock and waste. The results indicate that man-made emissions can be reduced sufficiently to limit methane-caused climate warming by 2100 even in the case of an uncontrolled natural Arctic methane emission feedback. This will however require a committed, global effort towards substantial, but feasible reductions.
In essence, we want to convey the message that the release of methane from human activities is something we can do something about, especially since the technology for drastic reductions is readily available - often even at a low cost. If we can only get the human emissions under control, the natural emissions should not have to be of major concern, concludes Höglund-Isaksson.
An inevitable warm-up for Earth
http://www.colorado.edu/today/2017/07/31/inevitable-warm-earthAn inevitable warm-up for Earth
Published: July 31, 2017
Even if humans could instantly turn off all emissions of greenhouse gases, Earth would continue to heat up about two more degrees Fahrenheit by the turn of the century, according to a sophisticated new analysis published today in the journal Nature Climate Change.
If current emission rates continue for 15 years, the research shows, odds are good that the planet will see nearly three degrees Fahrenheit (1.5 Celsius) of warming by then.
This committed warming is critical to understand because it can tell us and policymakers how long we have, at current emission rates, before the planet will warm to certain thresholds, said Robert Pincus, a scientist with the Cooperative Institute for Research in Environmental Sciences (CIRES), a partnership of the University of Colorado Boulder and NOAA. The window of opportunity on a 1.5-degree [C] target is closing.
During United Nations meetings in Paris last year, 195 countries including the United States signed an agreement to keep global temperature rise less than 3.5 degrees F (2 C) above pre-industrial levels, and pursue efforts that would limit it further, to less than 3 degrees Fahrenheit (1.5 C) by 2100.
http://dx.doi.org/10.1038/NCLIMATE3357
Methane-eating microbes found beneath Antarctica's melting ice sheets
http://news.ufl.edu/articles/2017/07/methane-eating-microbes-found-beneath-antarcticas-melting-ice-sheets-.phpMethane-eating microbes found beneath Antarctica's melting ice sheets
July 31, 2017
Rachel Damiani
photographer: Reed Scherer
Lurking in a lake half a mile beneath Antarcticas icy surface, methane-eating microbes may mitigate the release of this greenhouse gas into the atmosphere as ice sheets retreat.
A new study published today in Nature Geoscience traces methanes previously unknown path below the ice in a spot that was once thought to be inhospitable to life. Study researchers sampled the water and sediment in Antarcticas subglacial Whillans Lake by drilling 800 meters through ice for the first time ever. Next they measured methane amounts and used genomic analyses to find that 99 percent of methane released into the lake is gobbled up by microbes.
These tiny microorganisms may have a big impact on a warming world by preventing methane from seeping into the atmosphere when ice sheets melt, said Brent Christner, a University of Florida microbiologist and co-author on the study.
This is an environment that most people look at and dont think it could ever really directly impact us, Christner said. But this is a process that could have climatic implications.
http://dx.doi.org/10.1038/ngeo2992
Methane not escaping into the atmosphere from Arctic Ocean
https://cage.uit.no/news/methane-not-escaping-into-the-atmosphere-arctic-ocean/[font size=5]Methane not escaping into the atmosphere from Arctic Ocean[/font]
[font size=4]Methane gas released from the Arctic seabed during the summer months leads to an increased methane concentration in the ocean. But surprisingly, very little of the climate gas rising up through the sea reaches the atmosphere.[/font]
[font size=3]Our results are exciting and controversial, says senior scientist Cathrine Lund Myhre from NILU Norwegian Institute for Air Research, who is cooperating with CAGE through MOCA project.
The results were published in Geophysical Research Letters.
The scientist performed simultaneous measurements close to seabed, in the ocean and in the atmosphere during an extensive ship and air campaign offshore Svalbard Archipelago in summer 2014. As of today, three independent models employing the marine and atmospheric measurements show that the methane emissions from the sea bed in the area did not significantly affect the atmosphere.
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http://dx.doi.org/10.1002/2016GL068999.
Why Has a Drop in Global CO2 Emissions Not Caused CO2 Levels in the Atmosphere to Stabilize?
This comes from the keepers of the Keeling Curve (note this is a blog post from 2016.)
https://scripps.ucsd.edu/programs/keelingcurve/2016/05/23/why-has-a-drop-in-global-co2-emissions-not-caused-co2-levels-in-the-atmosphere-to-stabilize/
May 23, 2016 | Rob Monroe

[font size=3]Note: Readers have asked why there has been no stabilization in the measured levels of the greenhouse gas carbon dioxide in the atmosphere when reported emissions of CO₂ have fallen. Scripps CO₂ Group Director Ralph Keeling gave this response:
Theres a pretty simple reason why the recent stabilization in global emissions hasnt caused CO₂ levels to stabilize. The ocean and land sinks for CO₂ currently offset only about 50 percent of the emissions. So the equivalent of 50 percent of the emissions is still accumulating in the atmosphere, even with stable emissions. To stabilize CO₂ levels would require roughly an immediate roughly 50 percent cut in emissions, at which point the remaining emissions would be fully offset by the sinks, at least for a while.
Eventually, additional emissions cuts would be required because the sinks will slowly lose their efficiency as the land and ocean start to saturate. A permanent stabilization at current levels therefore requires both an immediate 50-percent cut as well as a slow tapering thereafter, eventually approaching zero emissions. The recent stabilization in emissions might be viewed as a very small first step toward the required cuts.
Robert Monroe[/font][/font]
We're on the brink of mass extinction -- but there's still time to pull back
http://www.mcgill.ca/newsroom/channels/news/were-brink-mass-extinction-theres-still-time-pull-back-268427[font size=4]News
Both ominous and hopeful, a new report paints a picture of the value of biodiversity, the threats it faces and the window of opportunity we have to save species before its too late[/font]
Published: 31 May 2017
[font size=3]Imagine being a scuba diver and leaving your oxygen tank behind you on a dive. Or a mountain climber and abandoning your ropes. Or a skydiver and shedding your parachute. Thats essentially what humans are doing as we expand our footprint on the planet without paying adequate attention to impacts on other living things, according to researchers from the University of Minnesota and McGill University. Because we depend on plants and animals for food, shelter, clean air and water and more, anything we do that makes life harder for them eventually comes around to make life harder for us as well.
But, reporting with colleagues from around the world in this weeks special biodiversity issue of the scientific journal Nature, the researchers also note that all is not lost, and offer specific strategies for turning that tide before its too late.
Forest Isbell, of University of Minnesotas College of Biological Sciences, McGill biologist Andrew Gonzalez and coauthors from eight countries on four continents provided an overview of what we know and still need to learn about the impacts of habitat destruction, overhunting, the introduction of nonnative species, and other human activities on biodiversity. In addition, they summarized previous research on how biodiversity loss affects nature and the benefits nature provides for example, a recent study showing that reduced diversity in tree species in forests is linked to reduced wood production. Synthesizing findings of other studies, they estimated that the value humans derive from biodiversity is 10 times what every country in the world put together spends on conservation today suggesting that additional investments in protecting species would not only reduce biodiversity loss but provide economic benefit, too.
Human activities are driving the sixth mass extinction in the history of life on Earth, despite the fact that diversity of life enhances many benefits people reap from nature, such as wood from forests, livestock forage from grasslands, and fish from oceans and streams, said Isbell, who served as lead author the paper. It would be wise to invest much more in conserving biodiversity.
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http://dx.doi.org/10.1038/nature22899
James Hansen -- Carbon Tax and 100% Dividend -- No Alligator Shoes!
This comes from 2008: http://www.columbia.edu/~jeh1/mailings/2008/20080604_TaxAndDividend.pdf
[font size=3]The charts for my talk (Climate Threat to the Planet: Implications for Energy Policy) on 3 June 2008 at the PACON 2008 conference (Energy and Climate Change: Innovative Approaches to Solving Todays Problems) are available as a pdf http://www.columbia.edu/~jeh1/2008/HawaiiPACON_20080603.pdf
or powerpoint http://www.columbia.edu/~jeh1/2008/HawaiiPACON_20080603.ppt
The Carbon Tax and 100% Dividend chart warrants discussion. Tax and dividend is the policy complement that must accompany recognition of fossil carbon reservoir sizes for strategic solution of global warming (the physics: reservoir sizes imply the need to phase-out coal emissions promptly and quash unconventional fossil fuels).
Tax and 100% dividend can drive innovation and economic growth with a snowballing effect. Carbon emissions will plummet far faster than in top-down or Manhattan projects. A clean environment that supports all life on the planet can be restored.
Carbon tax and 100% dividend is spurred by the recent carbon cap discussion of Peter Barnes and others. Principles must be crystal clear and adhered to rigorously. A tax on coal, oil and gas is simple. It can be collected at the first point of sale within the country or at the last (e.g., at the gas pump), but it can be collected easily and reliably. You cannot hide coal in your purse; it travels in railroad cars that are easy to spot. Cap, in addition, is a euphemism that may do as much harm as good. The public is not stupid.
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NREL Raises Rooftop Photovoltaic Technical Potential Estimate
(Please note: This story comes from the National Renewable Energy Laboratory. Copyright concerns are nil.)
http://www.nrel.gov/news/press/2016/24662
[font size=4]New analysis nearly doubles previous estimates and shows U.S. building rooftops could generate close to 40 percent of national electricity sales[/font]
March 24, 2016
[font size=3]Analysts at the Energy Department's National Renewable Energy Laboratory (NREL) have used detailed light detection and ranging (LiDAR) data for 128 cities nationwide, along with improved data analysis methods and simulation tools, to update its estimate of total U.S. technical potential for rooftop photovoltaic (PV) systems. The analysis reveals a technical potential of 1,118 gigawatts (GW) of capacity and 1,432 terawatt-hours (TWh) of annual energy generation, equivalent to 39 percent of the nation's electricity sales.
This current estimate is significantly greater than that of a previous NREL analysis, which estimated 664 GW of installed capacity and 800 TWh of annual energy generation. Analysts attribute the new findings to increases in module power density, improved estimation of building suitability, higher estimates of the total number of buildings, and improvements in PV performance simulation tools.
The analysis appears in "Rooftop Solar Photovoltaic Technical Potential in the United States: A Detailed Assessment." (PDF) The report quantifies the technical potential for rooftop PV in the United States, which is an estimate of how much energy could be generated if PV systems were installed on all suitable roof areas.
To calculate these estimates, NREL analysts used LiDAR data, Geographic Information System methods, and PV-generation modeling to calculate the suitability of rooftops for hosting PV in 128 cities nationwide-representing approximately 23 percent of U.S. buildings-and provide PV-generation results for 47 of the cities. The analysts then extrapolated these findings to the entire continental United States. The result is more accurate estimates of technical potential at the national, state, and zip code level.
"This report is the culmination of a three-year research effort and represents a significant advancement in our understanding of the potential for rooftop PV to contribute to meeting U.S. electricity demand," said Robert Margolis, NREL senior energy analyst and co-author of the report.
Within the 128 cities studied, the researchers found that 83 percent of small buildings have a suitable location for PV installation, but only 26 percent of those buildings' total rooftop area is suitable for development. Because of the sheer number of this class of building across the country, however, small buildings actually provide the greatest combined technical potential. Altogether, small building rooftops could accommodate up to 731 GW of PV capacity and generate 926 TWh per year of PV energy-approximately 65 percent of the country's total rooftop technical potential. Medium and large buildings have a total installed capacity potential of 386 GW and energy generation potential of 506 TWh per year, approximately 35 percent of the total technical potential of rooftop PV.
"An accurate estimate of PV's technical potential is a critical input in the development of regional deployment plans," said Pieter Gagnon, an engineering analyst of solar policy and technoeconomics at NREL and lead author of the report. "Armed with this new data, municipalities, utilities, solar energy researchers, and other stakeholders will have a much-improved starting point for PV research and policymaking, both regionally and nationwide."
"It is important to note that this report only estimates the potential from existing, suitable rooftops, and does not consider the immense potential of ground-mounted PV," said Margolis. "Actual generation from PV in urban areas could exceed these estimates by installing systems on less suitable roof space, by mounting PV on canopies over open spaces such as parking lots, or by integrating PV into building facades. Further, the results are sensitive to assumptions about module performance, which are expected to continue improving over time."
Technical potential is an established reference point for renewable technologies. It quantifies the amount of energy that can be captured from a particular resource, considering resource availability and quality, technical system performance, and the physical availability of suitable area for development-without consideration of economic factors like return on investment or market factors such as policies, competition with other technologies, and rate of adoption.
NREL's work was supported by funding from the Energy Department's Office of Energy Efficiency and Renewable Energy in support of its SunShot Initiative. The SunShot Initiative is a collaborative national effort that aggressively drives innovation to make solar energy fully cost-competitive with traditional energy sources before the end of the decade. Through SunShot, the department supports efforts by private companies, universities, and national laboratories to drive down the cost of solar electricity to $0.06 per kilowatt-hour. Learn more at energy.gov/sunshot.
NREL is the U.S. Department of Energy's primary national laboratory for renewable energy and energy efficiency research and development. NREL is operated for the Energy Department by The Alliance for Sustainable Energy, LLC.
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Visit NREL online at www.nrel.gov[/font][/font]
Target atmospheric CO2: Where should humanity aim? - by James Hansen et al.
This is the origin of the goal of 350 ppm.
http://dx.doi.org/10.2174/1874282300802010217
[font face=Serif][center][font size=1]The Open Atmospheric Science Journal, 2008, 2, 217-231[/font][/center][br][hr][font size=5]Target Atmospheric CO₂: Where Should Humanity Aim?[/font]
[font size=4]James Hansen*,1,2, Makiko Sato1,2, Pushker Kharecha1,2, David Beerling3, Robert Berner4, Valerie Masson-Delmotte5, Mark Pagani4, Maureen Raymo6, Dana L. Royer7 and James C. Zachos8[/font]
[font size=2]1NASA/Goddard Institute for Space Studies, New York, NY 10025, USA
2Columbia University Earth Institute, New York, NY 10027, USA
3Department of Animal and Plant Sciences, University of Sheffield, Sheffield S10 2TN, UK
4Department of Geology and Geophysics, Yale University, New Haven, CT 06520-8109, USA
5Lab. Des Sciences du Climat et lEnvironnement/Institut Pierre Simon Laplace, CEA-CNRS-Universite de Versailles Saint-Quentin en Yvelines, CE Saclay, 91191, Gif-sur-Yvette, France
6Department of Earth Sciences, Boston University, Boston, MA 02215, USA
7Department of Earth and Environmental Sciences, Wesleyan University, Middletown, CT 06459-0139, USA
8Earth & Planetary Sciences Dept., University of California, Santa Cruz, Santa Cruz, CA 95064, USA[/font]
[font size=1]Abstract: Paleoclimate data show that climate sensitivity is ~3°C for doubled CO₂, including only fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks, is ~6°C for doubled CO₂ for the range of climate states between glacial conditions and ice-free Antarctica. Decreasing CO₂ was the main cause of a cooling trend that began 50 million years ago, the planet being nearly ice-free until CO₂ fell to 450 ± 100 ppm ; barring prompt policy changes, that critical level will be passed, in the opposite direction, within decades. If humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, paleoclimate evidence and ongoing climate change suggest that CO₂ will need to be reduced from its current 385 ppm to at most 350 ppm, but likely less than that. The largest uncertainty in the target arises from possible changes of non-CO₂ forcings. An initial 350 ppm CO₂ target may be achievable by phasing out coal use except where CO₂ is captured and adopting agricultural and forestry practices that sequester carbon. If the present overshoot of this target CO₂ is not brief, there is a possibility of seeding irreversible catastrophic effects.[/font]
[font size=2]Keywords: Climate change, climate sensitivity, global warming.[/font]
[font size=3]1. INTRODUCTION
Human activities are altering Earths atmospheric composition. Concern about global warming due to long-lived human-made greenhouse gases (GHGs) led to the United Nations Framework Convention on Climate Change |1| with the objective of stabilizing GHGs in the atmosphere at a level preventing dangerous anthropogenic interference with the climate system.
The Intergovernmental Panel on Climate Change |IPCC, |2|| and others |3| used several reasons for concern to estimate that global warming of more than 2-3°C may be dangerous. The European Union adopted 2°C above pre - industrial global temperature as a goal to limit human-made warming |4|. Hansen et al. |5| argued for a limit of 1°C global warming (relative to 2000, 1.7°C relative to pre - industrial time), aiming to avoid practically irreversible ice sheet and species loss. This 1°C limit, with nominal climate sensitivity of ¾°C per W/m² and plausible control of other GHGs |6|, implies maximum CO₂ ~ 450 ppm |5|.
Our current analysis suggests that humanity must aim for an even lower level of GHGs. Paleoclimate data and ongoing global changes indicate that slow climate feedback processes not included in most climate models, such as ice sheet disintegration, vegetation migration, and GHG release from soils, tundra or ocean sediments, may begin to come into play on time scales as short as centuries or less |7|. Rapid on-going climate changes and realization that Earth is out of energy balance, implying that more warming is in the pipe-line |8|, add urgency to investigation of the dangerous level of GHGs.
A probabilistic analysis |9| concluded that the long-term CO₂ limit is in the range 300-500 ppm for 25 percent risk tolerance, depending on climate sensitivity and non-CO₂ forcings. Stabilizing atmospheric CO₂ and climate requires that net CO₂ emissions approach zero, because of the long lifetime of CO₂ |10, 11|.
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