How many papers support this gap analysis?

3 papers from our local library contribute to this synthesis, with an average publication year of 2023.

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earth_science3 papersavg year 2023weak evidence

The long-term contributions and regulatory effects

Research gap analysis derived from 3 earth_science papers in our local library.

The gap

The long-term contributions and regulatory effects of glacier and snow meltwater remain insufficiently quantified. There is a need to quantify the impact of climate change on runoff in the Upper Yarkant River Basin.

Evidence profile

Sourced from the stated research gap and abstract of the source papers, classified as general, drawn from work published between 2018 and 2026, spanning 3 journals. Those papers have been cited 130 times in total.

Research trend

Established — well-defined area with open sub-problems.

Supporting evidence — 3 representative gaps

Regulation of runoff by snow and glacier meltwater in the Yarkant River Basin, Tarim Basin (2026) · DOAJ (DOAJ: Directory of Open Access Journals) · doi
The long-term contributions and regulatory effects of glacier and snow meltwater remain insufficiently quantified. There is a need to quantify the impact of climate change on runoff in the Upper Yarkant River Basin.
generalstated research gap
Keywords: long-term contributions regulatory effects glacier snow meltwater remain
The Role of Atmospheric Rivers in Extratropical and Polar Hydroclimate (2018) · Journal of Geophysical Research Atmospheres · cited 130× · doi
, water vapor content and precipitation) has not been fully studied, even though moistening of the polar atmosphere is both a key result and amplifier of Arctic warming and sea ice melt, and precipitation is key to the surface mass balance of polar sea ice and ice sheets.
generalabstractevidence 4/5
Keywords: precipitation polar water vapor content fully studied even though moistening atmosphere result amplifier arctic warming
Estimating the thermodynamic contribution of post-industrial warming to recent Greenland ice sheet surface mass loss (2026) · The Cryosphere · doi
The contribution of the change in background conditions relative to changes in regional circulation patterns has yet to be quantified. The impact of thermodynamic changes on recent ice sheet meltwater runoff is not well understood. The role of amplified Arctic warming in recent ice sheet surface mass loss is not well quantified.
generalstated research gapevidence 4/5
Keywords: contribution change background conditions relative changes regional circulation

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