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3. Introduce the Result Into Self-Attention

Author

Ye, Chengcheng

Subjects
Computer Science - Computer Vision and Pattern Recognition
Abstract

Traditional self-attention mechanisms in convolutional networks tend to use only the output of the previous layer as input to the attention network, such as SENet, CBAM, etc. In this paper, we propose a new attention modification method that tries to get the output of the classification network in advance and use it as a part of the input of the attention network. We used the auxiliary classifier proposed in GoogLeNet to obtain the results in advance and pass them into attention networks. we added this mechanism to SE-ResNet for our experiments and achieved a classification accuracy improvement of at most 1.94% on cifar100.

Published
2021

18. Late Oligocene monsoonal climate in the Lunpola Basin, central Tibetan Plateau: evidence from palaeosol records.

Author

Guo, Zengguang, Wu, Fuli, Fang, Xiaomin, Ye, Chengcheng, Yang, Yibo, Zan, Jinbo, Mao, Ziqiang, and Shen, Maohua

Subjects
OLIGOCENE Epoch, FOREST soils, PALEOPEDOLOGY, CHEMICAL weathering, LANDSCAPE changes, CLAY, MONSOONS
Abstract

The Asian monsoon affects the natural patterns of climate in China and its origin and evolution have been a matter of much debate in palaeoclimatology. Results from recent studies indicate that the Asian monsoon had reached the subtropical zone by at least c. 41 Ma and expanded to the central Tibetan Plateau during the Late Oligocene, although more geological evidence is required to confirm its spatial and temporal evolution. The well-developed Late Oligocene palaeosol in the Lunpola Basin, central Tibetan Plateau is an ideal material for addressing the issue. Observations of various climatic indicators suggest that these palaeosols were forest cinnamon soils, as shown by the compound Bt and Bk horizons, abundant clay coatings and carbonate nodules, and the diagnostic chemical composition of clays in the Bt horizon. A high chemical weather index, the Rb/Sr ratios and high contents of illite/smectite mixed-layer minerals show that these palaeosols experienced intense weathering and leaching during pedogenesis. The mean annual temperature and mean annual precipitation during the developmental period of the palaeosols were 10.4–14.8°C and 615–1128 mm, respectively, as estimated by empirical formulas, which are comparable with those of cinnamon soils in current monsoon climates. This study provides important independent evidence from palaeosols for studies of the evolution of the Asian monsoon. Supplementary material: The data about the clay chemical composition and climatic indicators of palaeosol and modern soils are available at https://doi.org/10.6084/m9.figshare.c.6850703 Thematic collection: This article is part of the Mesozoic and Cenozoic tectonics, landscape and climate change collection available at: https://www.lyellcollection.org/topic/collections/mesozoic-and-cenozoic-tectonics-landscape-and-climate-change [ABSTRACT FROM AUTHOR]

Published
2024
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23. S1505 Visual Summaries of Gastroenterology Guidelines Increase Clinicians' Exposure to and Knowledge of Guideline-Based Clinical Care

Author

Enunwa, Chidiebele, primary, Obineme, Chuma, additional, Hang, Thuy-Van P., additional, Ye, Chengcheng, additional, Veeramachaneni, Hima, additional, Yu, Michael Andrew, additional, Hans, Amneet, additional, Vachaparambil, Cicily, additional, Patel, Vaishali, additional, Brown, Jason M., additional, and Spicer, Jennifer O., additional

Published
2022
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32. Cover Image

Author

Yang, Yibo, primary, Ye, Chengcheng, additional, Yang, Rongsheng, additional, and Fang, Xiaomin, additional

Published
2021
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34. Cenozoic advance of the East Asian monsoon promoted weathering of the magnesium-rich southern China upper crust and its significance for global geochemical cycles of carbon and magnesium

Author

Yang, Yibo, primary, Galy, Albert, additional, Fang, Xiaomin, additional, France-Lanord, Christian, additional, Wan, Shiming, additional, Yang, Rongsheng, additional, Zhang, Jian, additional, Zhang, Ran, additional, Yang, Song, additional, Miao, Yunfa, additional, Liu, Yudong, additional, and Ye, Chengcheng, additional

Published
2021
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43. Revisiting clay‐sized mineral and elemental records of the silicate weathering history in the northern Tibetan Plateau during the late Cenozoic: The role of aeolian dust.

Author

Yang, Yibo, Ye, Chengcheng, Yang, Rongsheng, and Fang, Xiaomin

Subjects
*NATIVE element minerals, *MINERAL dusts, *DUST, *CENOZOIC Era, *PLATEAUS, *EOLIAN processes
Abstract

Exceedingly strong aeolian dust activity has occurred in inland Asia. Comparisons of the late Cenozoic sedimentation rates between aeolian and fluvial‐lacustrine sequences around the northern Tibetan Plateau suggest that aeolian process has played an important role in the erosion, weathering and deposition of sediment. However, recognizing dust as an important source in fluvial‐lacustrine sequences is a vital but difficult task. Here, clay‐sized mineral and elemental records of regional silicate weathering histories are revisited during the period of Asian dust expansion at ~9–8 Ma. The aeolian dust input from the Tianshan‐Altay Orogens into the Jiuquan Basin is identified using the Th/Sc ratio while that from the Qilian Shan into the Xining Basin is identified based on inconsistent fine‐grained silicate weathering proxies. Our study suggests that the use of appropriate dust provenance tracers and recognition of wind transport‐induced changes in dust grain size and chemistry can provide useful aeolian dust discrimination approaches. [ABSTRACT FROM AUTHOR]

Published
2021
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