Abstract The Randolph Glacier Inventory (RGI) is a globally complete collection of digital outlines of glaciers, excluding the ice sheets, developed to meet the needs of the Fifth Assessment of the Intergovernmental Panel on Climate Change for estimates of past and future mass balance. The RGI was created with limited resources in a short period.…
Journal of Glaciology Template
Write in a clean editor, then format for Journal of Glaciology in one click — DocuGuru applies the official Cambridge University Press template with numbered references and exports a submission-ready PDF plus the editable LaTeX source. Free to start.
About the Journal of Glaciology format
Journal of Glaciology is a peer-reviewed journal published by Cambridge University Press, covering Cryospheric studies and observations, Climate change and permafrost, Winter Sports Injuries and Performance.
| Publisher | Cambridge University Press |
|---|---|
| Reference style | Numbered Numbered — [1], [2] in the text [1] A. Smith, B. Jones, and C. Lee, A representative article title, Journal of Glaciology 12 (2023) 45–58.
Formats any DOI in the closest standard style — Journal of Glaciology has no published style definition, so this is an approximation. No sign-up. |
| Publishes research in | Cryospheric studies and observations Climate change and permafrost Winter Sports Injuries and Performance Landslides and related hazards Arctic and Antarctic ice dynamics |
| ISSN | 0022-1430 |
| Citation impact (2-yr) | 2.07 |
| h-index | 193 |
| i10-index | 4,616 |
| Total citations | 265,201 |
| Article processing charge | $1,471 |
| Open access | Yes |
| Top institutions publishing here | University of Washington |
| Journal website | www.cambridge.org |
| You get | A submission-ready PDF and the editable LaTeX source — ready to submit. |
Papers published in Journal of Glaciology per year
Citation impact of Journal of Glaciology by publication year
Citations each year’s papers have accumulated so far — the most recent years are still building up.
Most-cited papers in Journal of Glaciology
Abstract Water flowing in tubular channels inside a glacier produces frictional heat, which causes melting of the ice walls. However the channels also have a tendency to close under the overburden pressure. Using the equilibrium equation that at every cross-section as much ice is melted as flows in, differential equations are given for steady flow…
Abstract A review of in situ and remote-sensing data covering the ice shelves of the Antarctic Peninsula provides a series of characteristics closely associated with rapid shelf retreat: deeply embayed ice fronts; calving of myriad small elongate bergs in punctuated events; increasing flow speed; and the presence of melt ponds on the ice-shelf surface in…
Abstract Observations show that glaciers around the world are in retreat and losing mass. Internationally coordinated for over a century, glacier monitoring activities provide an unprecedented dataset of glacier observations from ground, air and space. Glacier studies generally select specific parts of these datasets to obtain optimal assessments of the mass-balance data relating to the…
Abstract A network of passages situated along three-grain intersections enables water to percolate through temperate glacier ice. The deformability of the ice allows the passages to expand and contract in response to changes in pressure, and melting of the passage walls by heat generated by viscous dissipation and carried by above-freezing water causes the larger…