The Jakobshanvs Effect

The Jakobshavns Effect may have been a significant factor in hastening the collapse of palaeo ice sheets with the advent of climatic warming after 18,000 years ago and may precipitate partial collapse of the present‐day Greenland and Antarctic Ice Sheets following CO2‐induced climatic warming in the decades ahead. The Jakobshavns Effect is observed today on Jakobshavns Glacier, which is located at 69°10′N on the west coast of Greenland. The Jakobshavns Effect is a group of positive feedback mechanisms which allow Jakobshavns Glacier to literally pull ice out of the Greenland Ice Sheet at a rate exceeding 7 km/a across a floating terminus 800 m thick and 6 km wide. The pulling power results from an imbalance of horizontal hydrostatic forces in ice and water columns at the grounding line of the floating terminus. Positive feedback mechanisms that sustain the rapid ice discharge rate are ubiquitous surface crevassing, high summer rates of surface melting, extending creep flow, progressive basal uncoupling, progressive lateral uncoupling, and rapid iceberg calving.

The Adaptation Effect in Bilingual People who Stutter: An Examination of the Oral-Motor Rehearsal Theory

The present study provided further information about stuttering among bilingual populations and attempted to assess the significance of repeated oral-motor movements during an adaptation task in two bilingual adults. This was accomplished by requesting that bilingual people who stutter to complete an adaptation task of the same written passage in two different languages. Explored was the following research question: In bilingual speakers who stutter, what is the effect of altering the oral-motor movements by changing the language of the passage read during an adaptation task? Two bilingual adults were each requested to complete an adaptation task consisting of 10 readings in two separate conditions. Participants 1 and 2 completed two conditions, each of which contained a separate passage. Condition B consisted of an adaptation procedure in which the participants read five successive readings in English followed by five additional successive readings in Language 1 (L1). Following the completion of the first randomly assigned condition, the participant was given a rest period of 30 minutes before beginning the remaining condition and passage. Condition A consisted of an adaptation procedure in which the participants read five successive readings in L1 followed by five additional successive readings in English. Results across participants, conditions, and languages indicated an atypical adaptation curve over 10 readings characterized by a dramatic increase in stuttering following a change of language. Closer examination of individual participants revealed differences in stuttering and adaptation among languages and conditions. Participants 1 and 2 demonstrated differences in adaptation and stuttering among languages. Participant 1 demonstrated an increase in stuttering following a change in language read in Condition B and a decrease in stuttering following a change in language read in Condition A. It is speculated that language proficiency contributed to the observed differences in stuttering following a change of language. Participant 2 demonstrated an increase in stuttering following a change in language read in Condition A and a minimal increase in stuttering following a change in language read in Condition B. It is speculated that a change in the oral-motor plan contributed to the increase in stuttering in Condition A. Collectively, findings from this exploratory study lend support to an interactive effect between language proficiency and a change in the oral-motor plan contributing to increased stuttering following a change of language during an adaptation task.