book
European Geosciencies Union special publication series
Katlenburg-Lindau, Germany
Copernicus Publications
Singh
O. N.
Fabian
P.
Atmospheric Ozone: A Millennium Issue
2003
en
Atmospheric Ozone
ISBN 978-3-936586-08-4
147
book
Berlin, Heidelberg
Springer-Verlag
Fabian
Peter
Dameris
Martin
Ozone in the Atmosphere: Basic Principles, Natural and Human Impacts
Peter Fabian and Martin Dameris provide a concise yet comprehensive overview of established scientific knowledge about ozone in the atmosphere. They present both ozone changes and trends in the stratosphere, as well as the effects of overabundance in the troposphere including the phenomenon of photosmog.Aspects such as photochemistry, atmospheric dynamics and global ozone distribution as well as various techniques for ozone measurement are treated. The authors outline the various causes for ozone depletion, the effects of ozone pollution and the relation to climate change.The book provides a handy reference guide for researchers active in atmospheric ozone research and a useful introduction for advanced students specializing in this field. Non-specialists interested in this field will also profit from reading the book.Peter Fabian can look back on a life-long active career in ozone research, having first gained international recognition for his measurements of the global distribution of halogenated hydrocarbons. He also pioneered photosmog investigations in the metropolitan areas of Munich, Berlin, Athens and Santiago de Chile, and his KROFEX facility provided controlled ozone fumigation of adult tree canopies for biologists to investigate the effects of ozone increases on forests. Besides having published a broad range of scientific articles, he has also been the author or editor of numerous books. From 2002 to 2005 he served the European Geosciences Union (EGU) as their first and Founding President.Martin Dameris is a prominent atmospheric modeler whose interests include the impacts of all kinds of natural and man-made disturbances on the atmospheric system. His scientific work focuses on the connections between ozone and climate changes. For many years he has been an active contributor to the WMO scientific ozone depletion assessments, which have been used to monitor the depletion and recovery of the ozone layer in accordance with the Montreal Protocol.
2014
en
Ozone in the Atmosphere
DOI: https://doi.org/10.1007/978-3-642-54099-8
ISBN 978-3-642-54098-1
144
bookSection
ISBN 978-3-642-00493-3
Tropical Rainforests and Agroforests under Global Change: Ecological and Socio-economic Valuations
Berlin, Heidelberg
Springer-Verlag
van Edig
Xenia
Schwarze
Stefan
Zeller
Manfred
Tscharntke
Teja
Leuschner
Christoph
Veldkamp
Edzo
Faust
Heiko
Guhardja
Edi
Bidin
Arifuddin
The robustness of indicator based poverty assessment tools in changing environments - empirical evidence from Indonesia
Eradicating poverty is one of the highest priorities of development policies. Besides the necessary improvement of peoples livelihoods, the reduction of poverty is believed to have a positive effect on the stability of the rainforest margins. Better-off households are furthermore less vulnerable to shocks caused by natural hazards.
2010
DOI: https://doi.org/10.1007/978-3-642-00493-3_9
191-211
computerProgram
Randall
David
Dazlich
Donald
Heikes
Ross
Konor
Celal
CSU model for DCMIP 2016
2017
Zenodo
DOI: https://doi.org/10.5281/zenodo.580099
conferencePaper
DOI https://doi.org/10.5194/egusphere-egu2020-18622
Online
Buiter
S.
How syn-rift sedimentation promotes the formation of hyper-extended margins
Seismic observations show that some rifted continental margins may have substantial amounts of offshore sediments. For example, sediment layers of several kilometres thick are found on the margins of Mid Norway, Namibia and Angola. Intriguingly, these margins are wide, being characterised by distances of several hundreds of kilometres from typical continental crustal thicknesses of 30-40 km to clearly identifiable oceanic crust. On the other hand, some margins that are sediment-starved, such as Goban Spur, Flemish Cap and Northern Norway, have short onshore-to-offshore transitions. Variations in the amount of sediments not only impact the development of offshore sedimentary basins, but the changes in mass balance by erosion and sedimentation can also interact with extensional tectonic processes. In convergent settings, such feedback relationships between erosion and tectonic deformation have long been highlighted: Erosion reduces the elevation and width of mountain belts and in turn tectonic activity and exhumation are focused at regions of enhanced erosion. But what is the role played by surface processes during formation of rifted continental margins?
I use geodynamic finite-element experiments to explore the response of continental rifts to erosion and sedimentation from initial rifting to continental break-up. The experiments predict that rifted margins with thick syn-rift sedimentary packages are more likely to form hyper-extended crust and require more stretching to achieve continental break-up than sediment-starved margins. These findings imply that surface processes can control the style of continental break-up and that the role of sedimentation in rifted margin evolution goes far beyond the simple exertion of a passive weight.
4-8 May 2020
EGU2020-18622
Event-date: 4-8 May 2020
EGU General Assembly 2020
conferencePaper
Proceedings of the 6th International School
Garchim, Germany
Iwata
M.
Matsumoto
H.
Kojima
H.
Büchner
J.
Dum
C. T.
Scholer
M.
Büchner
J.
Dum
C. T.
Scholer
M.
Computer experiments on the plasma wave generation in the vicinity of Earths bow shock
3-8 September 2001
Event-date: 3-8 September 2001
4-6
Symposium on Space Plasma Simulation Overview
document
Pangaea
Heuer
Verena B.
Inagaki
F.
Morono
Yuki
Kubo
Y.
Spivack
Arthur J.
Viehweger
Bernhard
Treude
Tina
Beulig
F.
Schubotz
Florence
Tonai
S.
Bowden
S. A.
Cramm
M.
Henkel
Susann
Hirose
Takehiro
Homola
K.
Hoshino
Tatsuhiko
Ijiri
Akira
Imachi
H.
Kamiya
N.
Kaneko
Masanori
Lagostina
Lorenzo
Manners
Hayley
McClelland
H. L. O.
Metcalfe
K.
Okutsu
N.
Pan
Delu
Raudsepp
M. J.
Sauvage
Justine
Tsang
M. Y.
Wang
D. T.
Whitaker
E.
Yamamoto
Yuhji
Maeda
Lena
Adhikari
Rishi Ram
Glombitza
Clemens
Hamada
Y.
Kallmeyer
Jens
Wendt
J.
Wörmer
Lars
Yamada
Y.
Kinoshita
Masataka
Hinrichs
Kai-Uwe
Microbial abundance and activity at IODP Site C0023, Nankai Trough subduction zone
This data set documents data for a publication currently under consideration at Science. It documents data obtained for IODP Site C0023 during IODP Expedition 370. The data include: concentration of microbial cells and concentration of endospores in sediments, concentration and isotopic composition of methane and acetate in interstitial waters.
2020
Pangaea
Type: dataset
DOI: https://doi.org/10.1594/PANGAEA.923088
document
EUMETSAT
Loew
A.
Surface Albedo Validation Sites
2015
EUMETSAT
Type: dataset
DOI: https://doi.org/10.1594/PANGAEA.923088
document
University of Bristol
Rust
Alison
Cashman
Katharine
Liu
Emma
2011 Grímsvötn eruption: table of ash shape parameters
This dataset contains raw size measurements and derived shape parameters for six ash samples of the 2011 Grímsvötn eruption, Iceland (G1, G3, G4, G6, G7, & G8). All size measurements were made on backscattered electron SEM images using ImageJ image analysis software. Size measurements have units of pixels, and the dimensions of each pixels (in microns) is given for each sample. This dataset forms part of the supplementary material for the publication Liu, E.J., Cashman, K.V., Rust, A.C., & Gislason, S., (2015), The role of bubbles in generating fine ash during hydromagmatic eruptions', Geology.
2015
eng
University of Bristol
Type: dataset
DOI: https://doi.org/10.5523/bris.765l15d6gbsj1vty17u2a8ky2
Version: 1.0
journalArticle
20
Atmospheric Chemistry and Physics
DOI https://doi.org/10.5194/acp-20-15443-2020
23
Atmos. Chem. Phys.
Barker
P. A.
Allen
G.
Gallagher
M.
Pitt
J. R.
Fisher
R. E.
Bannan
T.
Nisbet
E. G.
Bauguitte
S. J. B.
Pasternak
D.
Cliff
S.
Schimpf
M. B.
Mehra
A.
Bower
K. N.
Lee
J. D.
Coe
H.
Percival
C. J.
Airborne measurements of fire emission factors for African biomass burning sampled during the MOYA campaign
2020
15443-15459
document
Jung
Martin
Koirala
Sujan
Weber
Ulrich
Ichii
Kazuhito
Gans
Fabian
Gustau Camps
Valls
Papale
Dario
Schwalm
Christopher
Tramontana
Gianluca
Reichstein
Markus
Computer Science - Machine Learning
Physics - Atmospheric and Oceanic Physics
Statistics - Machine Learning
The FLUXCOM ensemble of global land-atmosphere energy fluxes
Although a key driver of Earth's climate system, global land-atmosphere energy fluxes are poorly constrained. Here we use machine learning to merge energy flux measurements from FLUXNET eddy covariance towers with remote sensing and meteorological data to estimate net radiation, latent and sensible heat and their uncertainties. The resulting FLUXCOM database comprises 147 global gridded products in two setups: (1) 0.0833${\deg}$ resolution using MODIS remote sensing data (RS) and (2) 0.5${\deg}$ resolution using remote sensing and meteorological data (RS+METEO). Within each setup we use a full factorial design across machine learning methods, forcing datasets and energy balance closure corrections. For RS and RS+METEO setups respectively, we estimate 2001-2013 global (${\pm}$ 1 standard deviation) net radiation as 75.8${\pm}$1.4 ${W\ m^{-2}}$ and 77.6${\pm}$2 ${W\ m^{-2}}$, sensible heat as 33${\pm}$4 ${W\ m^{-2}}$ and 36${\pm}$5 ${W\ m^{-2}}$, and evapotranspiration as 75.6${\pm}$10 ${\times}$ 10$^3$ ${km^3\ yr^{-1}}$ and 76${\pm}$6 ${\times}$ 10$^3$ ${km^3\ yr^{-1}}$. FLUXCOM products are suitable to quantify global land-atmosphere interactions and benchmark land surface model simulations.
2018/12/11/
arxiv.org
arXiv:1812.04951
Type: article
document
Porter
J. G.
De Bruyn
W.
Saltzman
E. S.
Eddy flux measurements of sulfur dioxide deposition to the sea surface
13/06/2018
Atmos. Chem. Phys. Discuss.
Type: article
DOI: https://doi.org/10.5194/acp-18-15291-2018
map
Geological Survey of Canada, Open File 2490
Canada
Natural Resources Canada
Monger
J. W. H.
Journeay
J. M.
Guide to the geology and tectonic evolution of the southern Coast Mountains
1994
DOI: https://doi.org/10.4095/194829
1:500,000
thesis
Germany
Technische Universität Braunschweig
Kronberg
Elena Aleksandrovna
Dynamics of the Jovian magnetotail
The Jupiter orbiting spacecraft Galileo has provided evidence that the Jovian magnetotail is subject to a periodic process with a typical timescale of several days by which the Jovian system is presumably releasing its excess iogenic mass. This process is analyzed using data returned from the Energetic Particles Detector (EPD), the magnetometer and plasma wave experiment on Galileo. The mass release process resembles a terrestrial substorm in the sense of a global reconfiguration of the magnetotail. During the initial "loading" phase the plasma convection is at a moderate speed in the corotational direction, and the Jovian plasma sheet appears to be in a stable configuration. In the release phase reconnection through a thinned current sheet leads to radially inward and outward plasma flows and the ejection of plasmoids. The striking difference from terrestrial substorms is the periodical appearance of the reconfiguration events. Such an intrinsic periodic behavior cannot readily be explained by a solar wind driven process. Therefore the role of the solar wind as energy source is of less importance than for terrestrial substorms. Instead, ion mass-loading from internal plasma sources and fast planetary rotation causes stretching of magnetotail field lines. The resulting magnetotail configuration favors magnetic reconnection. This leads to the formation and release of plasmoids. Continued mass-loading then again leads to stretching of tail field lines. Thus assuming that this quasi-periodical process is internally driven, a simple conceptual model to estimate the time period of the periodic reconfiguration process is constructed. The model shows that the suggested intrinsic mechanism can explain the observed several days periodicities of Jovian substorm-like processes.
2006
DOI: https://doi.org/10.24355/dbbs.084-200608040200-26
133
PhD Thesis
webpage
Copernicus Publications
2018
https://publications.copernicus.org/
2018-10-25