Progress in Earth and Planetary Science

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PEPS出版論文を引用する際の
ジャーナル名略称:

Prog Earth Planet Sci

※Progress in Earth and Planetary Science は,公益社団法人日本地球惑星科学連合(JpGU)が運営する英文電子ジャーナルで,JpGUに参加する51学協会と協力して出版しています.

※Progress in Earth and Planetary Science は,独立行政法人日本学術振興会JSPSより科学研究費助成事業(科学研究費補助金)のサポートを受けています.

>>日本地球惑星科学連合

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  • Progress in Earth and Planetary Science
  • Progress in Earth and Planetary Science
  • Progress in Earth and Planetary Science
  • Progress in Earth and Planetary Science
  • Progress in Earth and Planetary Science
Progress in Earth and Planetary Science

Impact Factor 2.676

CiteScore 2.85

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Progress in Earth and Planetary Science (PEPS)とは?

  • 日本地球惑星科学連合(JpGU)が運営し,参加51学協会と協力して発行する査読付きオープンアクセスジャーナルで,読者は無料で自由に閲覧できます.
  • 地球惑星科学の全分野,および分野を超えたテーマに関する論文を扱います.

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11. Projection and impact assessment of global change

Schedule

Submission start: June 1, 2019

Submission deadline: December 31, 2019

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detail

Proponents:

Michio Kawamiya (Japan Agency for Marine-Earth Science and Technology, Japan)

Associate Editors:

Tatsuo Suzuki (Japan Agency for Marine-Earth Science and Technology, Japan)

Masayoshi Ishii (Meteorological Research Institute, Japan Meteorological Agency, Japan)

Kenji Tanaka (DPRI, Kyoto University, Japan)

Roy Rasmussen (National Center for Atmospheric Research, USA)

Anthropogenic forcings on global environment are expected to cause intensification of extreme events, sea level rise, ocean acidification, as well as large-scale ecosystem changes. The CMIP6 experimental protocol has been established, based on which modeling groups across the world are starting to provide environmental projection data toward 6th IPCC assessment report due in 2021. Various new types of studies, such as event attribution and coupling of socio-economic processes and Earth system dynamics, are also emerging in the field of global change projection. In addition, impact assessment studies using downscaling technique are becoming increasingly more important for grasping the significance of environmental changes for our society. Interactions and collaborations beyond boundaries of conventional scientific disciplines are desired for dealing with the issues of global change.

In this special issue SPEPS, we invite authors to contribute latest researches or reviews on global change from disciplinary and interdisciplinary viewpoints. The scope ranges over, but not limited to, development of climate/Earth system models, their applications on projections on global and regional scales, impact assessments with a particular emphasis on Asia, and cross-cutting studies with social scientists.

10. Stratigraphy and paleoclimatic/paleoenviromental evolution across the Early–Middle Pleistocene* transition in the Chiba composite section, Japan, and other reference sections in East Asia

Schedule

Submission start: September 1, 2018

Submission deadline: September 30, 2019

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detail

Proponents:

Yusuke Suganuma (National Institute of Polar Research, Japan)

Martin J. Head (Brock University, Canada)

Liping Zhou (Peking University, China)

Ryuji Tada (The University of Tokyo, Japan)

Takuya Sagawa (Kanazawa University, Japan)

Associate Editors:

Yusuke Suganuma (National Institute of Polar Research, Japan)

Martin J. Head (Brock University, Canada)

Takuya Sagawa (Kanazawa University, Japan)

The Earth experienced dramatic changes in oceanic and atmospheric circulation, ice sheet distributions, and biotic evolution from the Early to Middle Pleistocene. This interval is now known as the “Early–Middle Pleistocene transition (EMPT)” (Head and Gibbard, 2015). East Asia is an important region for land–ocean–atmosphere heat and moisture exchange owing to its location at the boundary between Eurasia and the Pacific Ocean. Understanding paleoenvironmental change in this region will therefore provide valuable insights into Earth’s climate system.

Continuous deep-ocean records across climatic transitions are not rare, but constructing detailed links to atmospheric circulation, terrestrial environmental change, and evolution of the biota has been hampered by a scarcity of continuous and expanded sedimentary records from coastal, shallow-marine environments. The Chiba composite section, a candidate for the Global Boundary Stratotype Section and Point (GSSP) to define the base of the Middle Pleistocene Subseries/Subepoch and newly proposed Chibanian Stage/Age, has a well-established chronology tied to the Matuyama–Brunhes reversal, providing a rare opportunity to capture terrestrial and marine environmental variability across Marine Isotope Stage 19 and hence the Lower–Middle Pleistocene boundary.

This special issue focuses on sedimentary records from the Chiba composite section and its stratigraphic correlation with other reference sections in East Asia. It addresses terrestrial and marine paleoclimatic and paleo-environmental co-evolution with emphasis on the mid-latitude westerly jet stream, East Asian monsoon, North Pacific Gyre, and the interplay of subtropical and subpolar settings through the Early–Middle Pleistocene transition.

*capitalization is needed to be consistent with the purpose of the special issue, which is to promote the Chiba section as the GSSP candidate for both the Chibanian Stage and the Middle Pleistocene Subseries.