[Vision2020] 10-30-17 World Meteorological Association: “severe ecological and economic disruptions,” said the report.

Ted Moffett starbliss at gmail.com
Tue Oct 31 20:38:44 PDT 2017


>From body of text below:

“CO2 remains in the atmosphere for hundreds of years and in the oceans for
even longer. The laws of physics mean that we face a much hotter, more
extreme climate in the future. There is currently no magic wand to remove
this CO2 from the atmosphere,” said Mr Taalas.
----------------------------
https://public.wmo.int/en/media/press-release/greenhouse-gas-concentrations-surge-new-record

Greenhouse gas concentrations surge to new record

30 October 2017

Concentrations of carbon dioxide in the atmosphere surged at a
record-breaking speed in 2016 to the highest level in 800 000 years,
according to the World Meteorological Organization's Greenhouse Gas Bulletin
<https://ane4bf-datap1.s3-eu-west-1.amazonaws.com/wmocms/s3fs-public/ckeditor/files/GHG_Bulletin_13_EN_final_1_1.pdf?LGJNmHpwKkEG2Qw4mEQjdm6bWxgWAJHa>.
The abrupt changes in the atmosphere witnessed in the past 70 years are
without precedent.

Globally averaged concentrations of CO2 reached 403.3 parts per million in
2016, up from 400.00 ppm in 2015 because of a combination of human
activities and a strong El Niño event. Concentrations of CO2 are now 145%
of pre-industrial (before 1750) levels, according to the Greenhouse Gas
Bulletin.

Rapidly increasing atmospheric levels of CO2 and other greenhouse gases
have the potential to initiate unprecedented changes in climate systems,
leading to “severe ecological and economic disruptions,” said the report.

The annual bulletin is based on observations from the WMO Global Atmosphere
Watch Programme. These observations help to track the changing levels of
greenhouse gases and serve as an early warning system for changes in these
key atmospheric drivers of climate change.

Population growth, intensified agricultural practices, increases in land
use and deforestation, industrialization and associated energy use from
fossil fuel sources have all contributed to increases in concentrations of
greenhouse gases in the atmosphere since the industrial era, beginning in
1750.

Since 1990, there has been a 40% increase in total radiative forcing – the
warming effect on our climate - by all long-lived greenhouse gases, and a
2.5% increase from 2015 to 2016 alone, according to figures from the US
National Oceanic and Atmospheric Administration quoted in the bulletin.

“Without rapid cuts in CO2 and other greenhouse gas emissions, we will be
heading for dangerous temperature increases by the end of this century,
well above the target set by the Paris climate change agreement,” said WMO
Secretary-General Petteri Taalas. “Future generations will inherit a much
more inhospitable planet, “ he said.

“CO2 remains in the atmosphere for hundreds of years and in the oceans for
even longer. The laws of physics mean that we face a much hotter, more
extreme climate in the future. There is currently no magic wand to remove
this CO2 from the atmosphere,”said Mr Taalas.

The last time the Earth experienced a comparable concentration of CO2  was
3-5 million years ago, the temperature was 2-3°C warmer and sea level was
10-20 meters higher than now.

The WMO Greenhouse Gas Bulletin reports on atmospheric concentrations  of
greenhouse gases. Emissions represent what goes into the atmosphere.
Concentrations represent what remains in the atmosphere after the complex
system of interactions between the atmosphere, biosphere, cryosphere and
the oceans. About a quarter of the total emissions is taken up by the
oceans and another quarter by the biosphere, reducing in this way the
amount of CO2 in the atmosphere.

A separate Emissions Gap Report by UN Environment, to be released on 31
October, tracks the policy commitments made by countries to reduce
greenhouse gas emissions and analyses how these policies will translate
into emissions reductions through 2030, clearly outlining the emissions gap
and what it would take to bridge it.

"The numbers don't lie. We are still emitting far too much and this needs
to be reversed. The last few years have seen enormous uptake of renewable
energy, but we must now redouble our efforts to ensure these new low-carbon
technologies are able to thrive. We have many of the solutions already to
address this challenge. What we need now is global political will and a new
sense of urgency," said Erik Solheim, head of UN Environment.

Together, the Greenhouse Gas Bulletin and Emissions Gap Report provide a
scientific base for decision-making at the UN climate change negotiations,
which will be held from 7-17 November in Bonn, Germany.

WMO, UN Environment and other partners are working towards an Integrated
Global Greenhouse Gas Information System to provide information that can
help nations to track the progress toward implementation of their national
emission pledges, improve national emission reporting and inform additional
mitigation actions. This system builds on the long-term experience of WMO
in greenhouse gas instrumental measurements and atmospheric modelling.

WMO is also striving to improve weather and climate services for the
renewable energy sector and to support the Green Economy and sustainable
development. To optimize the use of solar, wind and hydropower production,
new types of weather, climate and hydrological services are needed.

*Key findings of the Greenhouse Gas Bulletin*

*Carbon dioxide*

CO2  is by far the most important anthropogenic long-lived greenhouse gas.
Globally averaged concentrations for CO2 reached 403.3 parts per million in
2016, up from 400.00 ppm in 2015. This record annual increase of 3.3 ppm
was partly due to the strong 2015/2016 El Niño, which triggered droughts in
tropical regions and reduced the capacity of “sinks” like forests,
vegetation and the oceans to absorb CO2.   Concentrations of CO2 are now
145% of pre-industrial (before 1750) levels.

The rate of increase of atmospheric CO2 over the past 70 years is nearly
100 times larger than that at the end of the last ice age. As far as direct
and proxy observations can tell, such abrupt changes in the atmospheric
levels of CO2 have never before been seen.

<https://ane4bf-datap1.s3-eu-west-1.amazonaws.com/wmocms/s3fs-public/ckeditor/files/pr_1.jpg?U6l.CLdanuj2uD88NhjQnCzEb.HU.AqG>

Over the last 800 000 years, pre-industrial atmospheric CO2 content
remained below 280 ppm, but it has now risen to the 2016 global average of
403.3 ppm.

>From the most-recent high-resolution reconstructions from ice cores, it is
possible to observe that changes in CO2 have never been as fast as in the
past 150 years. The natural ice-age changes in CO2 have always preceded
corresponding temperature changes. Geological records show that the current
levels of CO2 correspond to an “equilibrium” climate last observed in the
mid-Pliocene (3–5 million years ago), a climate that was 2–3 °C warmer,
where the Greenland and West Antarctic ice sheets melted and even some of
the East Antarctic ice was lost, leading to sea levels that were 10–20 m
higher than those today.

*Methane*

Methane (CH4) is the second most important long-lived greenhouse gas and
contributes about 17% of radiative forcing. Approximately 40% of methane is
emitted into the atmosphere by natural sources (e.g., wetlands and
termites), and about 60% comes from human activities like cattle breeding,
rice agriculture, fossil fuel exploitation, landfills and biomass burning.

Atmospheric methane reached a new high of about 1 853 parts per billion
(ppb) in 2016 and is now 257% of the pre-industrial level.

*Nitrous Oxide *

Nitrous oxide (N2O) is emitted into the atmosphere from both natural (about
60%) and anthropogenic sources (approximately 40%), including oceans, soil,
biomass burning, fertilizer use, and various industrial processes.

Its atmospheric concentration in 2016 was 328.9 parts per billion. This is
122% of pre-industrial levels. It also plays an important role in the
destruction of the stratospheric ozone layer which protects us from the
harmful ultraviolet rays of the sun. It accounts for about 6% of radiative
forcing by long-lived greenhouse gases.

<https://ane4bf-datap1.s3-eu-west-1.amazonaws.com/wmocms/s3fs-public/ckeditor/files/pr_2.jpg?C1XOKj4Rrs3mF.CFHG11ZVXaqgKXq3SP>

For further information contact: Clare Nullis, media officer. Email
cnullis at wmo.int. Tel + 41 22 730 84 78 or Cell + 41 79 709 13 97

*Notes for Editors*

*The **WMO Global Atmosphere Watch Programme*
<http://www.wmo.int/gaw>*  coordinates
systematic observations and analysis of greenhouse gases and other trace
species. Fifty one countries contributed data for the Greenhouse Gas
Bulletin. Measurement data are reported by participating countries and
archived and distributed by the World Data Centre for Greenhouse Gases
<http://ds.data.jma.go.jp/gmd/wdcgg/> (WDCGG) at the Japan Meteorological
Agency.*

<https://ane4bf-datap1.s3-eu-west-1.amazonaws.com/wmocms/s3fs-public/ckeditor/files/pr_1.jpg?U6l.CLdanuj2uD88NhjQnCzEb.HU.AqG>
<https://ane4bf-datap1.s3-eu-west-1.amazonaws.com/wmocms/s3fs-public/ckeditor/files/pr_1.jpg?U6l.CLdanuj2uD88NhjQnCzEb.HU.AqG>
---------------------------------------
Vision2020 Post: Ted Moffett
***** Original material contained herein is Copyright 2000 through life
plus 70 years, Ted Moffett.  Do not copy, forward, excerpt, or reproduce
outside the Vision2020.Moscow.com <http://vision2020.moscow.com/>
forum without the express written permission of the author.*****
-------------- next part --------------
An HTML attachment was scrubbed...
URL: <http://mailman.fsr.com/pipermail/vision2020/attachments/20171031/1dedd0e8/attachment-0001.html>


More information about the Vision2020 mailing list