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Critical issues in trace gas biogeochemistry and global change

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Critical issues in trace gas biogeochemistry and global change. / Beerling, David J.; Hewitt, C. N.; Pyle, John A. et al.
In: Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences, Vol. 365, No. 1856, 07.2007, p. 1629-1642.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Beerling, DJ, Hewitt, CN, Pyle, JA & Raven, JA 2007, 'Critical issues in trace gas biogeochemistry and global change', Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences, vol. 365, no. 1856, pp. 1629-1642. https://doi.org/10.1098/rsta.2007.2037

APA

Beerling, D. J., Hewitt, C. N., Pyle, J. A., & Raven, J. A. (2007). Critical issues in trace gas biogeochemistry and global change. Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences, 365(1856), 1629-1642. https://doi.org/10.1098/rsta.2007.2037

Vancouver

Beerling DJ, Hewitt CN, Pyle JA, Raven JA. Critical issues in trace gas biogeochemistry and global change. Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences. 2007 Jul;365(1856):1629-1642. doi: 10.1098/rsta.2007.2037

Author

Beerling, David J. ; Hewitt, C. N. ; Pyle, John A. et al. / Critical issues in trace gas biogeochemistry and global change. In: Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences. 2007 ; Vol. 365, No. 1856. pp. 1629-1642.

Bibtex

@article{cf977977970f4d709d86ad97cded4251,
title = "Critical issues in trace gas biogeochemistry and global change",
abstract = "The atmospheric composition of trace gases and aerosols is determined by the emission of compounds from the marine and terrestrial biospheres, anthropogenic sources and their chemistry and deposition processes. Biogenic emissions depend upon physiological processes and climate, and the atmospheric chemistry is governed by climate and feedbacks involving greenhouse gases themselves. Understanding and predicting the biogeochemistry of trace gases in past, present and future climates therefore demands an interdisciplinary approach integrating across physiology, atmospheric chemistry, physics and meteorology. Here, we highlight critical issues raised by recent findings in all of these key areas to provide a framework for better understanding the past and possible future evolution of the atmosphere. Incorporating recent experimental and observational findings, especially the influence of CO2 on trace gas emissions from marine algae and terrestrial plants, into earth system models remains a major research priority. As we move towards this goal, archives of the concentration and isotopes of N2O and CH4 from polar ice cores extending back over 650 000 years will provide a valuable benchmark for evaluating such models. In the Pre-Quaternary, synthesis of theoretical modelling with geochemical and palaeontological evidence is also uncovering the roles played by trace gases in episodes of abrupt climatic warming and ozone depletion. Finally, observations and palaeorecords across a range of timescales allow assessment of the Earth's climate sensitivity, a metric influencing our ability to decide what constitutes 'dangerous' climate chan-e. 0",
keywords = "atmospheric composition, climate change, methane, isoprene, ozone, palaeoclimates, CARBON-ISOTOPE EXCURSION, EOCENE THERMAL MAXIMUM, ISOPRENE EMISSIONS, METHANE BUDGET, ATMOSPHERIC METHANE, COLUMN OBSERVATIONS, POSITIVE FEEDBACK, CLIMATE-CHANGE, NITROUS-OXIDE, SURFACE OCEAN",
author = "Beerling, {David J.} and Hewitt, {C. N.} and Pyle, {John A.} and Raven, {John A.}",
year = "2007",
month = jul,
doi = "10.1098/rsta.2007.2037",
language = "English",
volume = "365",
pages = "1629--1642",
journal = "Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences",
issn = "1364-503X",
publisher = "Royal Society of London",
number = "1856",

}

RIS

TY - JOUR

T1 - Critical issues in trace gas biogeochemistry and global change

AU - Beerling, David J.

AU - Hewitt, C. N.

AU - Pyle, John A.

AU - Raven, John A.

PY - 2007/7

Y1 - 2007/7

N2 - The atmospheric composition of trace gases and aerosols is determined by the emission of compounds from the marine and terrestrial biospheres, anthropogenic sources and their chemistry and deposition processes. Biogenic emissions depend upon physiological processes and climate, and the atmospheric chemistry is governed by climate and feedbacks involving greenhouse gases themselves. Understanding and predicting the biogeochemistry of trace gases in past, present and future climates therefore demands an interdisciplinary approach integrating across physiology, atmospheric chemistry, physics and meteorology. Here, we highlight critical issues raised by recent findings in all of these key areas to provide a framework for better understanding the past and possible future evolution of the atmosphere. Incorporating recent experimental and observational findings, especially the influence of CO2 on trace gas emissions from marine algae and terrestrial plants, into earth system models remains a major research priority. As we move towards this goal, archives of the concentration and isotopes of N2O and CH4 from polar ice cores extending back over 650 000 years will provide a valuable benchmark for evaluating such models. In the Pre-Quaternary, synthesis of theoretical modelling with geochemical and palaeontological evidence is also uncovering the roles played by trace gases in episodes of abrupt climatic warming and ozone depletion. Finally, observations and palaeorecords across a range of timescales allow assessment of the Earth's climate sensitivity, a metric influencing our ability to decide what constitutes 'dangerous' climate chan-e. 0

AB - The atmospheric composition of trace gases and aerosols is determined by the emission of compounds from the marine and terrestrial biospheres, anthropogenic sources and their chemistry and deposition processes. Biogenic emissions depend upon physiological processes and climate, and the atmospheric chemistry is governed by climate and feedbacks involving greenhouse gases themselves. Understanding and predicting the biogeochemistry of trace gases in past, present and future climates therefore demands an interdisciplinary approach integrating across physiology, atmospheric chemistry, physics and meteorology. Here, we highlight critical issues raised by recent findings in all of these key areas to provide a framework for better understanding the past and possible future evolution of the atmosphere. Incorporating recent experimental and observational findings, especially the influence of CO2 on trace gas emissions from marine algae and terrestrial plants, into earth system models remains a major research priority. As we move towards this goal, archives of the concentration and isotopes of N2O and CH4 from polar ice cores extending back over 650 000 years will provide a valuable benchmark for evaluating such models. In the Pre-Quaternary, synthesis of theoretical modelling with geochemical and palaeontological evidence is also uncovering the roles played by trace gases in episodes of abrupt climatic warming and ozone depletion. Finally, observations and palaeorecords across a range of timescales allow assessment of the Earth's climate sensitivity, a metric influencing our ability to decide what constitutes 'dangerous' climate chan-e. 0

KW - atmospheric composition

KW - climate change

KW - methane

KW - isoprene

KW - ozone

KW - palaeoclimates

KW - CARBON-ISOTOPE EXCURSION

KW - EOCENE THERMAL MAXIMUM

KW - ISOPRENE EMISSIONS

KW - METHANE BUDGET

KW - ATMOSPHERIC METHANE

KW - COLUMN OBSERVATIONS

KW - POSITIVE FEEDBACK

KW - CLIMATE-CHANGE

KW - NITROUS-OXIDE

KW - SURFACE OCEAN

U2 - 10.1098/rsta.2007.2037

DO - 10.1098/rsta.2007.2037

M3 - Journal article

VL - 365

SP - 1629

EP - 1642

JO - Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences

JF - Philosophical Transactions of the Royal Society A: Mathematical, Physical & Engineering Sciences

SN - 1364-503X

IS - 1856

ER -