ArticleNature communications2025
Modulation of inter-hemispheric temperature gradients on the Holocene Asian-Australian summer monsoon.
Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.
What it found
Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.
The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
The trial behind it
Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.
Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.
Who cites it
1 citing paper in PubMed.
- The Australian-Indonesian monsoon through time.National science review · 2026Review
Corrections and comments
PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.
Authors and funding
8 authors.
Funding
Abstract
The Asian-Australian monsoon system (A-AuMS) is the most typical cross-equatorial monsoon system and thus inter-hemispheric comparison is essential to explore its dynamics. Although the evolution of Holocene Asian summer monsoon has been extensively studied, changes in Australian summer monsoon (AuSM) is less investigated due to the lack of identified high-resolution paleoclimate records. Here we obtain a 13.5 kyr AuSM record from lacustrine sediments in northeastern Australia. It suggests that the weakening of the AuSM during the early to middle Holocene was regulated by Northern Hemisphere high-latitude ice volume, while the strengthening of the AuSM during the middle to late Holocene was mainly controlled by increased Southern Hemisphere summer insolation. The combination of Asian and Australian monsoon records show that the coupling evolution of A-AuMS was dominated by the temperature gradient between two hemispheres, which involve the changes of the AMOC, Northern Hemisphere ice volumes and solar insolation in both hemispheres.
Identifiers
What OpenQuestion holds
Registered trials
Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.