Global Warming: some back-of-the-envelope calculations

We do several simple calculations and measurements in an effort to gain understanding of global warming and the carbon cycle. Some conclusions are interesting: (i) There has been global warming since the end of the "little ice age" around 1700. There is no statistically significant evidenc...

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Main Authors: Fabara, C, Hoeneisen, B
Language:English
Published: 2005
Subjects:
Online Access:http://cds.cern.ch/record/827750
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spelling ftcern:oai:cds.cern.ch:827750 2023-05-15T16:39:12+02:00 Global Warming: some back-of-the-envelope calculations Fabara, C Hoeneisen, B 2005-03-14 http://cds.cern.ch/record/827750 eng eng http://cds.cern.ch/record/827750 physics/0503119 USFQ-2005-39 oai:cds.cern.ch:827750 Other Fields of Physics 2005 ftcern 2018-07-28T07:17:04Z We do several simple calculations and measurements in an effort to gain understanding of global warming and the carbon cycle. Some conclusions are interesting: (i) There has been global warming since the end of the "little ice age" around 1700. There is no statistically significant evidence of acceleration of global warming since 1940. (ii) The increase of CO_2 in the atmosphere, beginning around 1940, accurately tracks the burning of fossil fuels. Burning all of the remaining economically viable reserves of oil, gas and coal over the next 150 years or so will approximately double the pre-industrial atmospheric concentration of CO_2. The corresponding increase in the average temperature, due to the greenhouse effect, is quite uncertain: between 1.3 and 4.8K. This increase of temperature is (partially?) offset by the increase of aerosols and deforestation. (iii) Ice core samples indicate that the pre-historic CO_2 concentration and temperature are well correlated. We conclude that changes in the temperatures of the oceans are probably the cause of the changes of pre-historic atmospheric CO_2 concentration. (iv) Data suggests that large volcanic explosions can trigger transitions from glacial to interglacial climates. (v) Most of the carbon fixed by photosynthesis in the Amazon basin returns to the atmosphere due to aerobic decay. Other/Unknown Material ice core CERN Document Server (CDS)
institution Open Polar
collection CERN Document Server (CDS)
op_collection_id ftcern
language English
topic Other Fields of Physics
spellingShingle Other Fields of Physics
Fabara, C
Hoeneisen, B
Global Warming: some back-of-the-envelope calculations
topic_facet Other Fields of Physics
description We do several simple calculations and measurements in an effort to gain understanding of global warming and the carbon cycle. Some conclusions are interesting: (i) There has been global warming since the end of the "little ice age" around 1700. There is no statistically significant evidence of acceleration of global warming since 1940. (ii) The increase of CO_2 in the atmosphere, beginning around 1940, accurately tracks the burning of fossil fuels. Burning all of the remaining economically viable reserves of oil, gas and coal over the next 150 years or so will approximately double the pre-industrial atmospheric concentration of CO_2. The corresponding increase in the average temperature, due to the greenhouse effect, is quite uncertain: between 1.3 and 4.8K. This increase of temperature is (partially?) offset by the increase of aerosols and deforestation. (iii) Ice core samples indicate that the pre-historic CO_2 concentration and temperature are well correlated. We conclude that changes in the temperatures of the oceans are probably the cause of the changes of pre-historic atmospheric CO_2 concentration. (iv) Data suggests that large volcanic explosions can trigger transitions from glacial to interglacial climates. (v) Most of the carbon fixed by photosynthesis in the Amazon basin returns to the atmosphere due to aerobic decay.
author Fabara, C
Hoeneisen, B
author_facet Fabara, C
Hoeneisen, B
author_sort Fabara, C
title Global Warming: some back-of-the-envelope calculations
title_short Global Warming: some back-of-the-envelope calculations
title_full Global Warming: some back-of-the-envelope calculations
title_fullStr Global Warming: some back-of-the-envelope calculations
title_full_unstemmed Global Warming: some back-of-the-envelope calculations
title_sort global warming: some back-of-the-envelope calculations
publishDate 2005
url http://cds.cern.ch/record/827750
genre ice core
genre_facet ice core
op_relation http://cds.cern.ch/record/827750
physics/0503119
USFQ-2005-39
oai:cds.cern.ch:827750
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