Kaihe Yamazaki

ORCID: 0000-0003-3631-5365
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About
Contact & Profiles
Research Areas
  • Arctic and Antarctic ice dynamics
  • Geology and Paleoclimatology Research
  • Oceanographic and Atmospheric Processes
  • Cryospheric studies and observations
  • Methane Hydrates and Related Phenomena
  • Climate variability and models
  • Marine and coastal ecosystems
  • Atmospheric and Environmental Gas Dynamics
  • Geological Studies and Exploration
  • Winter Sports Injuries and Performance
  • Heart Rate Variability and Autonomic Control
  • Aerospace Engineering and Energy Systems
  • Handwritten Text Recognition Techniques
  • Food Industry and Aquatic Biology
  • Biomedical and Chemical Research
  • Biofield Effects and Biophysics
  • Geomagnetism and Paleomagnetism Studies
  • Ergonomics and Musculoskeletal Disorders
  • Skin Protection and Aging
  • Ocean Acidification Effects and Responses
  • Image Processing and 3D Reconstruction
  • Sleep and Work-Related Fatigue
  • Adolescent Sexual and Reproductive Health
  • Optical measurement and interference techniques
  • Balance, Gait, and Falls Prevention

University of Tasmania
2023-2025

Australian Antarctic Division
2023-2025

Australian Centre for Excellence in Antarctic Science
2023-2025

Hokkaido University
2020-2024

National Institute of Polar Research
2022-2024

Kogakuin University
2024

Scripps Institution of Oceanography
2024

University of California, San Diego
2024

Tokyo University of Marine Science and Technology
2022

Hokkaido University of Science
2022

Poleward expansion of the Antarctic Circumpolar Current warms continental margin.

10.1126/sciadv.abf8755 article EN cc-by Science Advances 2021-06-11

The Totten Glacier in East Antarctica, with an ice volume equivalent to >3.5 m of global sea-level rise, is grounded below sea level and, therefore, vulnerable ocean forcing. Here, we use bathymetric and oceanographic observations from previously unsampled parts the continental shelf reveal on-shelf warm water pathways defined by deep topographic features. Access Ice Shelf (TIS) cavity facilitated a break, broad depression on shelf, cyclonic circulation that carries inner troughs provide...

10.1038/s41467-023-39764-z article EN cc-by Nature Communications 2023-08-17

Full-depth hydrographic sections of the BROKE experiment in 1996 (across Antarctic margin from 80 to 150°E; Bindoff et al., 2000) were revisited for first time during 2018/2019 austral summer. We describe subsurface physical oceanography 2019 and changes between not documented earlier studies. The survey captured decadal ocean structure southern flank Circumpolar Current (ACC) continental shelves. In five cross-slope meridional sections, where measurements are comparable (112, 120, 128, 140,...

10.1016/j.pocean.2024.103285 article EN cc-by Progress In Oceanography 2024-05-24

Dense, cold waters formed on Antarctic continental shelves descend along the margin, where they mix with other Southern Ocean to form Bottom Water (AABW). AABW then spreads into deepest parts of all major ocean basins, isolating heat and carbon from atmosphere for centuries. Despite AABW’s key role in regulating Earth’s climate long time scales recording conditions, remains poorly observed. This lack observational data is mostly due two factors. First, originates shelf slope situ...

10.3389/fmars.2023.1221701 article EN cc-by Frontiers in Marine Science 2023-12-08

Abstract Melting ice shelves around Antarctica control the massive input of freshwater into ocean and play an intricate role in global heat redistribution. The Amery Ice Shelf regulates wintertime sea-ice growth dense shelf water formation. We investigated warm Antarctic Surface Water melting its impact on water. Here we show that coastal summer 2016/17 was almost free, leading to higher surface temperatures. glacial meltwater fraction highest record, hypothesised be attributable anomalous...

10.1038/s43247-022-00456-z article EN cc-by Communications Earth & Environment 2022-06-22

Abstract The advent of under‐ice profiling float and biologging techniques has enabled year‐round observation the Southern Ocean its Antarctic margin. These data are often overlooked in widely used oceanographic datasets, despite their importance understanding seasonality role sea ice changes, water mass formation, glacial melt. We develop a monthly climatology (south 40°S above 2,000 m) using Data Interpolating Variational Analysis, which excels multi‐dimensional interpolation consistent...

10.1029/2024jc020920 article EN cc-by Journal of Geophysical Research Oceans 2025-01-01

Objectives: Wheelchair seat sagging is hypothesized to increase pressure and shear forces, potentially leading injuries. The objective of this study was assess the impact correcting wheelchair on ischial pressure, force, posture in a population healthy adults. Methods: Twenty-four adults, meeting specific anthropometric requirements for proper fit, were recruited. Participants evaluated under two conditions: with base correction (With Correction) without it (No Correction). Correction...

10.20944/preprints202502.2141.v1 preprint EN 2025-02-26

Abstract The Antarctic continental margin supplies the densest bottom water to global abyss. From late twentieth century, an acceleration in long-term freshening of Bottom Waters (AABW) has been detected Australian-Antarctic Basin. Our latest hydrographic observations reveal that, 2010s, trend reversed broadly over slope. Near-bottom salinities 2018–2019 were higher than during 2011–2015. Along 170° E, salinity increase between 2011 and 2018 was greater that observed west. layer thickness...

10.1038/s41598-020-71290-6 article EN cc-by Scientific Reports 2020-09-15

Abstract The climatological structure of the subpolar cyclonic circulation off East Antarctica is delineated with Argo float data from past decade. Up to 40% profiles in seasonal ice zone have been without satellite positioning. We refined their position as following bathymetry get appropriate positions continental margin. error terrain‐following interpolation was estimated by using positioned be 23 ± 27 (78 70) km for 90 (390) day period. Profiles under‐ice period shorter than 360 days are...

10.1029/2019jc015406 article EN Journal of Geophysical Research Oceans 2020-07-07

Abstract To quantitatively assess the inorganic carbon cycle in eastern Indian sector of Southern Ocean (80–150°E, south 60°S), we measured ocean surface temperature, salinity, total alkalinity (TA), partial pressure dioxide (pCO 2 ), and concentrations chlorophyll‐ a (chl dissolved (DIC), nutrients during KY18 survey (December 2018–January 2019). The sea–air CO flux this region was −8.3 ± 12.7 mmol m −2 day −1 (−92.1 to +10.6 ). therefore weak sink. Based on DIC TA temperature minimum...

10.1029/2021jc017953 article EN cc-by Journal of Geophysical Research Oceans 2021-12-18

Abstract Warm, salty Circumpolar Deep Water (CDW) is recognized as the primary driver for Antarctic glacial melt, but mechanism by which it reaches continental shelves remains highly uncertain from an observational standpoint. With scarcity of eddy flux estimation in margin, we quantify isopycnal diffusivity CDW using hydrographic variability and satellite altimetry under mixing length framework. For comparison, spiciness thickness are used tracers, two tracers yield qualitatively similar...

10.1029/2022jc019422 article EN cc-by Journal of Geophysical Research Oceans 2023-02-01

The interbasin exchange between the Sea of Okhotsk and North Pacific governs intermediate water ventilation fertilization nutrient-rich subpolar Pacific, thus has an enormous influence on Pacific. However, mechanism this is puzzling; current studies have not explained how western boundary (WBC) subarctic intrudes only partially into Okhotsk. High-resolution models often exhibit unrealistically small exchanges, as WBC overshoots passing by deep straits does induce flows. Therefore, partial...

10.1038/s41598-021-91412-y article EN cc-by Scientific Reports 2021-06-08

Abstract The recent discovery of warm ocean water near the Totten Ice Shelf (TIS) has increased attention to Sabrina Coast in East Antarctica. We report result 6‐day helicopter‐based observations conducted during 61st Japanese Antarctic Research Expedition (JARE61), revealing (0.5–1°C) occupying a large previously unsampled area (116.5°E−120°E) below 550–600 m. Along TIS front, we observe modified Circumpolar Deep Water (mCDW) well above freezing (∼−0.7°C), consistent with previous work....

10.1029/2022gl097864 article EN cc-by-nc Geophysical Research Letters 2023-09-11

Abstract To clarify the impacts of basal melting Antarctic ice sheet and biological productivity on biogeochemical processes in coastal waters, concentrations dissolved inorganic carbon (DIC), total alkalinity (TA), nutrients, chlorophyll a , stable oxygen isotopic ratios (δ 18 O) were measured from offshore slope to front Totten Ice Shelf (TIS) during spring/summer 2018, 2019, 2020. Modified Circumpolar Deep Water (mCDW) intruded onto continental shelf off TIS flowed along bathymetric...

10.1029/2022gb007510 article EN cc-by Global Biogeochemical Cycles 2022-09-13

In East Antarctica, warm ocean water travels toward the Totten Ice Shelf. This melts and thins ice shelf, speeds up rate at which moves into sea, leading to sea-level rise. Scientists often get on board ships called icebreakers study in these regions. However, sea icebergs are major obstacles navigation scientific operations. For example, American, Australian, Japanese tried but could only observe a small area where was more broken up. So, we used helicopter measure during one of our...

10.3389/frym.2024.1080545 article EN Frontiers for Young Minds 2024-03-27

This paper presents a new method for identifying individuals using 2-dimensional joint coordinate data of periodic motion estimated with OpenPose. The proposed approach includes normalization technique depth-invariance and dissimilarity function lag-invariance that utilizes complex Fourier coefficients. To demonstrate the effectiveness method, experiments were conducted videos taken simultaneously at different depths.

10.1117/12.3053333 article EN 2024-10-21
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