English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

glacier, the sub-alpine niche glacier formed by abnormally heavy snowfalls and the drifted snow, but not including any kind of avalanche, and named it the "Mount Chokai type glacier" (TSUCHIYA, 1978b). During the period 1972-1981, yearly field surveys on the "Kaigata Glacieret," one of these types of glaciers, were carried out and the results showed several peculiar features of a very small glacier. Kaigata Glacieret was formed at about 1400m a. s. l., some 2000m below the so called climatic snowline, and covered about 0.04km2 during a one-year period of development, and then diminished to form tiny ice patches during the course of a few years. The estimated maximum snow depth at the site of this glacier at the end of a snowfall season was about 45m or more. The ablation rate is very high and the observed maximum rate during a warm rainstorm was 1.4cm/h. The rate of

A Very Small Glacier on Mt. Chokai, Japan, 1972-1981