Klimaatverandering (Dutch Wikipedia)

Analysis of information sources in references of the Wikipedia article "Klimaatverandering" in Dutch language version.

refsWebsite

Global rank Dutch rank

20web.archive.org

1^st place

6ipcc.ch

1,778^th place

2,370^th place

3worldcat.org

5^th place

28^th place

3nature.com

234^th place

128^th place

3doi.org

2^nd place

8^th place

2knmi.nl

5,147^th place

144^th place

2sciencemag.org

857^th place

261^st place

2cern.ch

1,959^th place

2,069^th place

1sciencedirect.com

149^th place

200^th place

1uu.nl

2,467^th place

184^th place

1wur.nl

8,218^th place

169^th place

1nasa.gov

75^th place

115^th place

1epa.gov

882^nd place

1,900^th place

1usgs.gov

167^th place

143^rd place

1eos.org

low place

1nih.gov

4^th place

12^th place

1google.nl

1,423^rd place

17^th place

1klimaatportaal.nl

low place

1ametsoc.org

4,162^nd place

3,929^th place

ametsoc.org

journals.ametsoc.org

M.J. Stevens en G.R. North (2006). Detection of the Climate Response to the Solar Cycle. Journal of the Atmospheric Sciences 53 (18).

cern.ch

press.web.cern.ch

CERN’s CLOUD experiment shines new light on climate change. CERN press office (6 oktober 2013). Gearchiveerd op 10 maart 2016.

cdsweb.cern.ch

(en) J Kirkby voor het CERN. Cosmic rays and climate, 4 juni 2009. Gearchiveerd op 14 maart 2023.

doi.org

dx.doi.org

(en) Zalasiewicz, Jan, Waters, Colin N., Williams, Mark, Barnosky, Anthony D., Cearreta, Alejandro (5 oktober 2015). When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal. Gearchiveerd op 24 mei 2019. Quaternary International 383: 196–203. ISSN:1040-6182. DOI:10.1016/j.quaint.2014.11.045.
(en) Foster, Gavin L., Royer, Dana L., Lunt, Daniel J. (4 april 2017). Future climate forcing potentially without precedent in the last 420 million years. Gearchiveerd op 17 augustus 2023. Nature Communications 8 (1): 14845. ISSN:2041-1723. DOI:10.1038/ncomms14845.

doi.org

(en) Mann, Michael E. (27 november 2009). Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly. Science 326 (5957): 1256-1260. ISSN: 0036-8075. PMID 19965474. DOI: 10.1126/science.1177303.

eos.org

Characterizing Interglacial Periods over the Past 800,000 Years. Gearchiveerd op 21 augustus 2020. Geraadpleegd op 11 januari 2020.

epa.gov

19january2017snapshot.epa.gov

(en) US EPA, OAR, Glossary of Climate Change Terms. 19january2017snapshot.epa.gov. Gearchiveerd op 18 augustus 2023. Geraadpleegd op 24 november 2022.

google.nl

books.google.nl

Erwin Kreyszig - Advanced engineering mathematics - Wiley 2006

ipcc.ch

(en) Allen, M. R.; Dube, O. P.; Solecki, W.; Aragón-Durand, F.; et al., . "Chapter 1: Framing and Context". (PDF). IPCC SR15 49–91. (2018). Gearchiveerd op 18 juli 2022. ""These global-level rates of human-driven change far exceed the rates of change driven by geophysical or biosphere forces that have altered the Earth System trajectory in the past e.g., Summerhayes, 2015; Foster et al., 2017); even abrupt geophysical events do not approach current rates of human-driven change.""
(en) Allen, M. R.; Dube, O. P.; Solecki, W.; Aragón-Durand, F.; et al., . "Chapter 1: Framing and Context". (PDF). IPCC SR15 49–91. (2018). Gearchiveerd op 18 juli 2022. ""These global-level rates of human-driven change far exceed the rates of change driven by geophysical or biosphere forces that have altered the Earth System trajectory in the past (e.g., Summerhayes, 2015; Foster et al., 2017); even abrupt geophysical events do not approach current rates of human-driven change.""
(en) V Masson-Delmotte en M Schulz voor het IPCC. Information from Paleoclimate Archives. In: Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the IPCC.
(en) Climate Change 2021: The Physical Science Basis. www.ipcc.ch. Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.
IPCC (2013). Fifth Assessment Report
(en) Myhre, G. et al., Antropogenic and natural radiative forcing. Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (2013). Gearchiveerd op 5 augustus 2023. ""There is very high confidence that industrial-era natural forcing is a small fraction of the anthropogenic forcing except for brief periods following large volcanic eruptions. In particular, robust evidence from satellite observations of the solar irradiance and volcanic aerosols demonstrates a near-zero (–0.1 to +0.1 W m–2) change in the natural forcing compared to the anthropogenic ERF increase of 1.0 (0.7 to 1.3) W m–2 from 1980 to 2011. The natural forcing over the last 15 years has likely offset a substantial fraction (at least 30%) of the anthropogenic forcing.""

klimaatportaal.nl

De rol van kosmische straling op Klimaatportaal.nl

knmi.nl

KNMI - Klimaatverandering. www.knmi.nl. Gearchiveerd op 4 november 2022. Geraadpleegd op 24 november 2022.
Koninklijk Nederlands Meteorologisch Instituut (KNMI), Kleine ijstijd. Gearchiveerd op 27 maart 2023.

nasa.gov

climate.nasa.gov

Shaftel, Holly, Overview: Weather, Global Warming and Climate Change. Climate Change: Vital Signs of the Planet. Gearchiveerd op 26 november 2022. Geraadpleegd op 24 november 2022.

nature.com

(en) Foster, Gavin L., Royer, Dana L., Lunt, Daniel J. (4 april 2017). Future climate forcing potentially without precedent in the last 420 million years. Gearchiveerd op 17 augustus 2023. Nature Communications 8 (1): 14845. ISSN:2041-1723. DOI:10.1038/ncomms14845.
Brajesh K. Singh, Richard D. Bardgett, Pete Smith & Dave S. Reay Microorganisms and climate change: terrestrial feedbacks and mitigation options Nature Reviews Microbiology 8 November 2010
Q. Schiermeier (2007). No solar hiding place for greenhouse sceptics. Nature 448 (8-9).

nih.gov

ncbi.nlm.nih.gov

(en) Mann, Michael E. (27 november 2009). Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly. Science 326 (5957): 1256-1260. ISSN: 0036-8075. PMID 19965474. DOI: 10.1126/science.1177303.

sciencedirect.com

(en) Zalasiewicz, Jan, Waters, Colin N., Williams, Mark, Barnosky, Anthony D., Cearreta, Alejandro (5 oktober 2015). When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal. Gearchiveerd op 24 mei 2019. Quaternary International 383: 196–203. ISSN:1040-6182. DOI:10.1016/j.quaint.2014.11.045.

sciencemag.org

(en) Mann, Michael E. (27 november 2009). Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly. Science 326 (5957): 1256-1260. ISSN: 0036-8075. PMID 19965474. DOI: 10.1126/science.1177303.

news.sciencemag.org

Katia Moskvitch, Do Cosmic Rays Grease Lightning? (3 mei 2013). Gearchiveerd op 25 december 2015.

usgs.gov

(en) How long can we expect the present Interglacial period to last?. www.usgs.gov. Geraadpleegd op 11 januari 2020.

uu.nl

Klimaatverandering - Dossiers - Universiteit Utrecht. www.uu.nl. Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.

web.archive.org

(en) Allen, M. R.; Dube, O. P.; Solecki, W.; Aragón-Durand, F.; et al., . "Chapter 1: Framing and Context". (PDF). IPCC SR15 49–91. (2018). Gearchiveerd op 18 juli 2022. ""These global-level rates of human-driven change far exceed the rates of change driven by geophysical or biosphere forces that have altered the Earth System trajectory in the past e.g., Summerhayes, 2015; Foster et al., 2017); even abrupt geophysical events do not approach current rates of human-driven change.""
(en) Zalasiewicz, Jan, Waters, Colin N., Williams, Mark, Barnosky, Anthony D., Cearreta, Alejandro (5 oktober 2015). When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal. Gearchiveerd op 24 mei 2019. Quaternary International 383: 196–203. ISSN:1040-6182. DOI:10.1016/j.quaint.2014.11.045.
(en) Foster, Gavin L., Royer, Dana L., Lunt, Daniel J. (4 april 2017). Future climate forcing potentially without precedent in the last 420 million years. Gearchiveerd op 17 augustus 2023. Nature Communications 8 (1): 14845. ISSN:2041-1723. DOI:10.1038/ncomms14845.
Klimaatverandering - Dossiers - Universiteit Utrecht. www.uu.nl. Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.
Klimaatverandering. WUR (6 september 2016). Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.
KNMI - Klimaatverandering. www.knmi.nl. Gearchiveerd op 4 november 2022. Geraadpleegd op 24 november 2022.
(en) Allen, M. R.; Dube, O. P.; Solecki, W.; Aragón-Durand, F.; et al., . "Chapter 1: Framing and Context". (PDF). IPCC SR15 49–91. (2018). Gearchiveerd op 18 juli 2022. ""These global-level rates of human-driven change far exceed the rates of change driven by geophysical or biosphere forces that have altered the Earth System trajectory in the past (e.g., Summerhayes, 2015; Foster et al., 2017); even abrupt geophysical events do not approach current rates of human-driven change.""
Shaftel, Holly, Overview: Weather, Global Warming and Climate Change. Climate Change: Vital Signs of the Planet. Gearchiveerd op 26 november 2022. Geraadpleegd op 24 november 2022.
(en) US EPA, OAR, Glossary of Climate Change Terms. 19january2017snapshot.epa.gov. Gearchiveerd op 18 augustus 2023. Geraadpleegd op 24 november 2022.
Characterizing Interglacial Periods over the Past 800,000 Years. Gearchiveerd op 21 augustus 2020. Geraadpleegd op 11 januari 2020.
De St. Bernardusabdij. Geschiedenis van Aduard.
Koninklijk Nederlands Meteorologisch Instituut (KNMI), Kleine ijstijd. Gearchiveerd op 27 maart 2023.
(en) Climate Change 2021: The Physical Science Basis. www.ipcc.ch. Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.
Katia Moskvitch, Do Cosmic Rays Grease Lightning? (3 mei 2013). Gearchiveerd op 25 december 2015.
CERN’s CLOUD experiment shines new light on climate change. CERN press office (6 oktober 2013). Gearchiveerd op 10 maart 2016.
UNEP/GRID Present Carbon Cycle
UNEP/GRID Emissions of CO₂ (1995)
(en) Myhre, G. et al., Antropogenic and natural radiative forcing. Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (2013). Gearchiveerd op 5 augustus 2023. ""There is very high confidence that industrial-era natural forcing is a small fraction of the anthropogenic forcing except for brief periods following large volcanic eruptions. In particular, robust evidence from satellite observations of the solar irradiance and volcanic aerosols demonstrates a near-zero (–0.1 to +0.1 W m–2) change in the natural forcing compared to the anthropogenic ERF increase of 1.0 (0.7 to 1.3) W m–2 from 1980 to 2011. The natural forcing over the last 15 years has likely offset a substantial fraction (at least 30%) of the anthropogenic forcing.""
C. de Jager, G.J.M. Versteegh en R. van Dorland (2006). Zongedreven klimaatveranderingen: een wetenschappelijke verkenning (WAB), KNMI, NIOZ.
(en) J Kirkby voor het CERN. Cosmic rays and climate, 4 juni 2009. Gearchiveerd op 14 maart 2023.

worldcat.org

(en) Zalasiewicz, Jan, Waters, Colin N., Williams, Mark, Barnosky, Anthony D., Cearreta, Alejandro (5 oktober 2015). When did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal. Gearchiveerd op 24 mei 2019. Quaternary International 383: 196–203. ISSN:1040-6182. DOI:10.1016/j.quaint.2014.11.045.
(en) Foster, Gavin L., Royer, Dana L., Lunt, Daniel J. (4 april 2017). Future climate forcing potentially without precedent in the last 420 million years. Gearchiveerd op 17 augustus 2023. Nature Communications 8 (1): 14845. ISSN:2041-1723. DOI:10.1038/ncomms14845.
(en) Mann, Michael E. (27 november 2009). Global Signatures and Dynamical Origins of the Little Ice Age and Medieval Climate Anomaly. Science 326 (5957): 1256-1260. ISSN: 0036-8075. PMID 19965474. DOI: 10.1126/science.1177303.

wur.nl

Klimaatverandering. WUR (6 september 2016). Gearchiveerd op 24 november 2022. Geraadpleegd op 24 november 2022.