マツオカ ノリカズ松岡 憲知特任教授Norikazu Matsuoka
■研究者基本情報
委員歴
- 2000年 - 2022年, Editorial board, Permafrost and Periglacial Processes
- 2011年 - 2017年, 編集委員, 東京地学協会
- 1998年 - 2016年, Co-chair, Periglacial Working group, International Permafrost Association
- 1993年 - 2016年, Full member, Commission on Cold and High Altitude Regions, International Geographical Union
- 1999年 - 2009年, Editorial Board, JAPANESE GEOMORPHOLOGICAL UNION
- 1999年 - 2009年, 編集幹事, 日本地形学連合
- 1998年 - 2007年, Editorial Board, THE ASSOCIATION JAPANESE GEOGRAPHERS
- 1998年 - 2007年, 編集専門委員, 日本地理学会
■研究活動情報
論文
- 〔主要な業績〕Decadal variability of differential frost heave on incipient sorted patterned ground in the Southern Japanese Alps
Norikazu Matsuoka, 筆頭著者
Permafrost and Periglacial Processes, 2025年04月, ［査読有り］ - 〔主要な業績〕Acceleration and interannual variability of creep rates in mountain permafrost landforms (rock glacier velocities) in the European Alps in 1995–2022
Andreas Kellerer-Pirklbauer; Xavier Bodin; Reynald Delaloye; Christophe Lambiel; Isabelle Gärtner-Roer; Mylène Bonnefoy-Demongeot; Luca Carturan; Bodo Damm; Julia Eulenstein; Andrea Fischer; Lea Hartl; Atsushi Ikeda; Viktor Kaufmann; Karl Krainer; Norikazu Matsuoka; Umberto Morra Di Cella; Jeannette Noetzli; Roberto Seppi; Cristian Scapozza; Philippe Schoeneich; Martin Stocker-Waldhuber; Emmanuel Thibert; Matteo Zumiani, Abstract
Cryospheric long-term timeseries get increasingly important. To document climate-related effects on long-term viscous creep of ice-rich mountain permafrost, we investigated timeseries (1995–2022) of geodetically-derived Rock Glacier Velocity (RGV), i.e. spatially averaged interannual velocity timeseries related to a rock glacier (RG) unit or part of it. We considered 50 RGV from 43 RGs spatially covering the entire European Alps. Eight of these RGs are destabilized. Results show that RGV are distinctly variable ranging from 0.04 to 6.23 m a−1. Acceleration and deceleration at many RGs are highly correlated with similar behaviour over 2.5 decades for 15 timeseries. In addition to a general long-term, warming-induced trend of increasing velocities, three main phases of distinct acceleration (2000–2004, 2008–2015, 2018–2020), interrupted by deceleration or steady state conditions, were identified. The evolution is attributed to climate forcing and underlines the significance of RGV as a product of the Essential Climate Variable (ECV) permafrost. We show that RGV data are valuable as climate indicators, but such data should always be assessed critically considering changing local factors (geomorphic, thermal, hydrologic) and monitoring approaches. To extract a climate signal, larger RGV ensembles should be analysed. Criteria for selecting new RGV-sites are proposed., IOP Publishing
Environmental Research Letters, 2024年02月20日, ［査読有り］ - Debris-flow activity in the Japanese Alps is controlled by extreme precipitation and ENSO – Evidence from multi-centennial tree-ring records
Juan Antonio Ballesteros-Cánovas; Yoshihiko Kariya; Fumitoshi Imaizumi; Alberto Muñoz Torrero Manchado; Ryoko Nishii; Norikazu Matsuoka; Markus Stoffel, Elsevier BV
Global and Planetary Change, 2023年12月, ［査読有り］ - 〔主要な業績〕How can needle ice transport large stones? Twenty‐one years of field observations
Norikazu Matsuoka, 筆頭著者, Abstract
Downslope movements of 12 stones (10–27 cm in diameter) were determined from time‐series images for 21 years on a Japanese alpine debris slope (inclination 12°). The process of stone movements was analysed on the basis of frost heave and soil temperature records, with particular attention to the stone size transported by needle ice and the effect of climate change on stone movements. Soil heaving mainly due to needle‐ice growth occurred 24–85 times yr−1 with an annual maximum and cumulative amounts of 1.8–5.5 cm and 17–58 cm yr−1, respectively. Stones moved downslope at rates of 5–20 cm yr−1 (mean 11.7 cm), the velocity correlating with the stone size, although small stones with a height of less than about 3 cm do not reduce needle‐ice activity very much. On an assumption of a linear relationship between the two variables, needle ice can transport stones with a diameter of as large as 30 cm. Both annual mean air/soil temperatures and needle‐ice activity slightly increased through the monitoring period. Climatic warming may have raised the frequency of needle ice by shortening the snow‐covered period., Wiley
Earth Surface Processes and Landforms, 2023年08月16日, ［査読有り］ - 〔主要な業績〕Ice needles weave patterns of stones in freezing landscapes
Anyuan Li; Norikazu Matsuoka; Fujun Niu; Jing Chen; Zhenpeng Ge; Wensi Hu; Desheng Li; Bernard Hallet; Johan van de Koppel; Nigel Goldenfeld; Quan-Xing Liu, Patterned ground, defined by the segregation of stones in soil according to size, is one of the most strikingly self-organized characteristics of polar and high-alpine landscapes. The presence of such patterns on Mars has been proposed as evidence for the past presence of surface liquid water. Despite their ubiquity, the dearth of quantitative field data on the patterns and their slow dynamics have hindered fundamental understanding of the pattern formation mechanisms. Here, we use laboratory experiments to show that stone transport is strongly dependent on local stone concentration and the height of ice needles, leading effectively to pattern formation driven by needle ice activity. Through numerical simulations, theory, and experiments, we show that the nonlinear amplification of long wavelength instabilities leads to self-similar dynamics that resemble phase separation patterns in binary alloys, characterized by scaling laws and spatial structure formation. Our results illustrate insights to be gained into patterns in landscapes by viewing the pattern formation through the lens of phase separation. Moreover, they may help interpret spatial structures that arise on diverse planetary landscapes, including ground patterns recently examined using the rover Curiosity on Mars., Proceedings of the National Academy of Sciences
Proceedings of the National Academy of Sciences, 2021年10月05日, ［査読有り］ - 〔主要な業績〕Interpreting rockfall activity on an outcrop-talus slope system in the southern Japanese Alps using an integrated survey approach
Fumitoshi Imaizumi; Daniel Trappmann; Norikazu Matsuoka; Juan Canovas Antonio Ballesteros; Koh Yasue; Markus Stoffel, ELSEVIER
GEOMORPHOLOGY, 2020年12月, ［査読有り］ - 〔主要な業績〕A multi-method monitoring of timing, magnitude and origin of rockfall activity in the Japanese Alps
Norikazu Matsuoka, 筆頭著者, A multi-method monitoring was conducted to detect the timing and trigger of rockfall activity on an alpine rockslide cliff composed of Cretaceous sandstone and shale in the southern Japanese Alps (Aresawa rockslide, 2900 m above sea level). The monitoring programme includes manual measurements of flaking from painted rock surface and collection of fallen debris, daily time-lapse imaging of the rockwall, automated recordings of rock temperature, rock moisture and influencing meteorological factors (air temperature and precipitation). A stereographic pair of sequential photographs is used to visually identify the location of new erosion and semi quantitative evaluation of detached materials at daily resolution. Six years (2010-2016) of debris trapping show major rockfall activity in winter (between November and May) and occasional activity associated with heavy rains in summer, and yield an average rate of rockwall retreat on the order of 1 mm a(-1). The rockwall shows heterogeneous debris production mainly reflecting joint spacing. Time-lapse imaging displays at least 10-15 rockfall events per year within the shot area (similar to 500 m(2)). The integration of multiple data suggests, Elsevier
Geomorphology, 2019年07月, ［査読有り］ - 〔主要な業績〕Ice-wedge polygon dynamics in Svalbard: Lessons from a decade of automated multi-sensor monitoring
Norikazu Matsuoka; Hannne H Christiansen; Tatsuya Watanabe, 筆頭著者, WILEY
PERMAFROST AND PERIGLACIAL PROCESSES, 2018年07月, ［査読有り］ - 〔主要な業績〕Interpretation of recent alpine landscape system evolution using geomorphic mapping and L-band InSAR analyses
Fumitoshi Imaizumi; Takaki Nishiguchi; Norikazu Matsuoka; Daniel Trappmann; Markus Stoffel, Elsevier B.V.
Geomorphology, 2018年06月01日, ［査読有り］ - 〔主要な業績〕Frost sorting on slopes by needle ice: A laboratory simulation on the effect of slope gradient
Anyuan Li; Norikazu Matsuoka; Fujun Niu, John Wiley and Sons Ltd
Earth Surface Processes and Landforms, 2018年03月15日, ［査読有り］ - 〔主要な業績〕Soil Physical and Environmental Conditions Controlling Patterned-Ground Variability at a Continuous Permafrost Site, Svalbard
Tatsuya Watanabe; Norikazu Matsuoka; Hanne H. Christiansen; Stefanie Cable
PERMAFROST AND PERIGLACIAL PROCESSES, 2017年04月, ［査読有り］ - Overview of the Special Issue "Rock Weathering from Nanoscale to Global Scale: 1. Microscopic Weathering and Basic Studies"
Norikazu MATSUOKA; Chiaki T OGUCHI; Keisuke FUKUSHI; Yuki MATSUSHI; Tadashi YOKOYAMA, 公益社団法人 東京地学協会
地學雜誌, 2017年 - 〔主要な業績〕岩石の物理的風化－実験・観測・自然現象のリンク－
松岡 憲知; 藁谷 哲也; 若狭 幸,Physical rock weathering has been studied through laboratory experiments, field observations, and numerical modeling, but linking these approaches and applying the results to weathering features in the field are often problematic. We review recent progress in three weathering processes—frost shattering, thermal fracturing, and lightning strikes—and explore better approaches to linking weathering processes and products. New visual and sensor technologies have led to great advances in field monitoring of weathering of fractured bedrock and resulting rockfalls in cold mountains. Laboratory simulations successfully produce fractures resulting from segregational freezing in various intact rocks. Modelling approaches illustrate the long-term evolution of periglacial slopes well, but improvements are required to apply laboratory-derived criteria to frost weathering. The efficacy of thermal weathering, which has long been under debate, is now partly supported by laboratory and field evidence that cracking takes place when wild fires or artificial explosions lead to thermal shock. Rock fracturing due to strong radiation is also reevaluated from the presence of large cooling/warmin, 公益社団法人 東京地学協会
地學雜誌, 2017年, ［査読有り］ - Biographical sketch of a giant: Deciphering recent debris-flow dynamics from the Ohya landslide body (Japanese Alps)
Fumitoshi Imaizumi; Daniel Trappmann; Norikazu Matsuoka; Satoshi Tsuchiya; Okihiro Ohsaka; Markus Stoffel
GEOMORPHOLOGY, 2016年11月, ［査読有り］ - 〔主要な業績〕Progress in understanding the dynamics, internal structure and palaeoenvironmental potential of ice wedges and sand wedges
Hanne H. Christiansen; Norikazu Matsuoka; Tatsuya Watanabe
PERMAFROST AND PERIGLACIAL PROCESSES, 2016年10月, ［査読有り］ - 〔主要な業績〕火星表面の永久凍土と周氷河作用
松岡 憲知, 筆頭著者, Following the development of high-resolution imaging, digital elevation models, thermal and hydrological data, and onsite ground information during the early period of the 21st century, the periglacial geomorphology of the Martian surface advanced rapidly. Images can even resolute meter-scale landforms, enabling identification of most periglacial features and analysis of their global distributions and detailed morphologies. This review focuses on progress in research covering permafrost distribution, patterned ground, possible heave and subsidence features, lobate debris forms, and slope-lineated features during the last decade. Most of the Martian high-latitude surface is underlain by ice-rich ground called the latitude-dependent mantle (LDM), which favors permafrost-related features possibly developed under warm-humid conditions during past high-obliquity periods or partially s,till active under the present cold-dry conditions. Thermal contraction cracking is likely to prevail in the LDM, resulting in high-centered, flat-top polygons, possibly underlain by sublimation-type wedges or sand wedges that prevail at high latitudes. The surface patterns change into subdued or peak-to, 東京地学協会
地学雑誌, 2016年02月, ［査読有り］ - 〔主要な業績〕Laboratory frost sorting by needle ice: a pilot experiment on the effects of stone size and extent of surface stone cover
Chizuru Yamagishi; Norikazu Matsuoka, 責任著者
EARTH SURFACE PROCESSES AND LANDFORMS, 2015年03月, ［査読有り］ - 〔主要な業績〕Combining Time-Lapse Photography and Multisensor Monitoring to Understand Frost Creep Dynamics in the Japanese Alps
Norikazu Matsuoka, 筆頭著者
PERMAFROST AND PERIGLACIAL PROCESSES, 2014年04月, ［査読有り］ - 〔主要な業績〕南アルプスにおける地形変動と土砂収支－最近の研究動向と展望－
松岡 憲知; 今泉 文寿; 西井 稜子, 筆頭著者, This review paper synthesizes geomorphic dynamics, sediment transport and resulting natural hazards in mountains of the southern Japanese Alps and their drainage basins, where climatic and geological situations produce highly active landform dynamics. In alpine areas above the timber line, shallow diurnal freeze-thaw action operating in the thin topsoil produces small-scale periglacial forms, and gravitational spreading leads to numerous sackung features where snow-melt and heavy rain in places promote rockslides. In subalpine and montane areas, deep-seated landslides originate from fractured sedimentary rocks, deep V-shaped valleys, and heavy rain, while shallow landslides continue with historical forest clearance. Continuous slope failures prevent vegetation recovery and maintain debris input to valleys. Steep valleys contribute to high-density debris flows. Frequent or repetitive occurrences of these mass movements promote continuous denudation of slopes, rockfall accidents along hiking trails, and sedimentation at artificial dams. They occasionally cause significant hazards to villages further downstream. Predicting and mitigating slope hazards require distinguishing among a, Tokyo Geographical Society
地学雑誌, 2013年08月, ［査読有り］ - 〔主要な業績〕Cold region geomorphology in Japan
Matsuoka; Norikazu, 筆頭著者, This paper reviews glacial and periglacial geomorphology and associated studies on physical geography and Quaternary geology, undertaken by Japanese researchers during the last three decades. Major progress has been achieved in two aspects. First, overseas fieldwork in a wide range of polar and alpine regions has promoted understanding of present-day glacier and permafrost landforms, processes and sediments. The outcomes have greatly influenced domestic research, improving the interpretation of past glaciation and periglaciation in Japan. Second, Japanese studies have made significant contributions to the international research communities in applying tephrochronology to dating tills and periglacial structures, proposing a distinct feature of glacial advances possibly reflecting climate conditions in eastern Asia, promoting comprehensive monitoring of periglacial processes and understanding periglacial processes in seasonal frost and marginal periglacial conditions., The Association of Japanese Geographers
Geographical Review of Japan, 2013年07月, ［査読有り］ - 〔主要な業績〕Precursors and triggers of an alpine rockslide in Japan: the 2004 partial collapse during a snow-melting period
Ryoko Nishii; Norikazu Matsuoka; Hiromu Daimaru; Masatsugu Yasuda
LANDSLIDES, 2013年02月, ［査読有り］ - 〔主要な業績〕Ice- and Soil-Wedge Dynamics in the Kapp Linne Area, Svalbard, Investigated by Two- and Three-Dimensional GPR and Ground Thermal and Acceleration Regimes
Tatsuya Watanabe; Norikazu Matsuoka; Hanne H. Christiansen
PERMAFROST AND PERIGLACIAL PROCESSES, 2013年01月, ［査読有り］ - 〔主要な業績〕Kinematics of an alpine retrogressive rockslide in the Japanese Alps
Ryoko Nishii; Norikazu Matsuoka
EARTH SURFACE PROCESSES AND LANDFORMS, 2012年12月, ［査読有り］ - 〔主要な業績〕MUDBOIL AND ICE-WEDGE DYNAMICS INVESTIGATED BY ELECTRICAL RESISTIVITY TOMOGRAPHY, GROUND TEMPERATURES AND SURFACE MOVEMENTS IN SVALBARD
Tatsuya Watanabe; Norikazu Matsuoka; Hanne H. Christiansen
GEOGRAFISKA ANNALER SERIES A-PHYSICAL GEOGRAPHY, 2012年12月, ［査読有り］ - Frost wedges as a periglacial climate indicator: reevaluation based on physical processes
Matsuoka, N, Elsevier
Quaternary International, 2012年11月 - Controls on patterned ground variability at a continuous permafrost site, Central Spitsbergen
Watanabe; T; Matsuoka; N; Christiansen; HH
Proceedings of the Tenth International Conference on Permafrost, 2012年08月, ［査読有り］ - 山岳地における崩壊地の拡大プロセス観測 : 赤石山脈アレ沢崩壊地を対象として
西井; 稜子; 松岡; 憲知, 砂防学会
砂防学会誌 : 新砂防 = Journal of the Japan Society of Erosion Control Engineering, 2012年01月 - 〔主要な業績〕周氷河地形プロセス研究最前線
松岡; 憲知; 池田; 敦, 筆頭著者, Periglacial process studies, which began in the mid-20th century, have greatly advanced in recent years following several breakthroughs. This paper reviews the latest breakthroughs supported by new technologies, themes, and international projects. New technologies have enabled small, high-resolution data loggers to monitor rock and soil movements, and thermal and hydrological properties in polar and alpine areas; enabled geophysical instruments to visualize two- and three- dimensional subsurface structures below periglacial features; and, enabled numerical simulations to predict future landform evolution. In particular, dramatic progress has been achieved in understanding bedrock shattering and falls, soil movements induced by freeze-thaw oscillations, controls on rock glacier creep, critical conditions for ice-wedge cracking, and biogeophysical impacts on non-sorted circles. Two key words, global warming and Mars, are appearing often in periglacial research. High mountains and polar lowlands face the fate of potential natural hazards associated with rock slides, debris flows and thermokarst subsidence, possibly originating from permafrost thawing. High-resolution orbital images, 東京地学協会
地学雑誌, 2012年01月, ［査読有り］ - 〔主要な業績〕スイスアルプスの周氷河環境と地形変動 : 15年間の観測の総括と展望
松岡; 憲知; 池田; 敦, 筆頭著者, Spacio-temporal variability of contemporary periglacial environments in the Swiss Alps is summarized on the basis of 15 years of field observations of rock weathering, permafrost creep, and soil movements, as well as other recent studies. Diurnal and annual freeze-thaw cycles loosen wet rock joints, which subsequently produce rockfalls. A large episodic rockfall can temporarily raise the rate of rockwall retreat. Rock debris derived from different parent rocks controls the types of rock glacier having different compositions, thermal characteristics, and dynamics. Some rock glaciers at the lower limit of permafrost are accelerating due to intensified mobility, but they may eventually become inactive because of permafrost thawing and the lack of debris supply. On slopes mantled with fine debris, small-scale stripes and lobes tend to develop on the upper part due to thin debris and good drainage, whereas larger scale lobes increase downslope as a result of thicker debris, poor drainage, and gentler slopes. The former mainly responds to shallow diurnal freeze-thaw cycles, whereas the latter reflects frost heave and gelifluction during deeper annual freezing-thawing. A prolonged supp, 東京地学協会
地学雑誌, 2011年06月, ［査読有り］ - 〔主要な業績〕Climate and material controls on periglacial soil processes: Toward improving periglacial climate indicators
Norikazu Matsuoka, 筆頭著者
QUATERNARY RESEARCH, 2011年03月, ［査読有り］ - 〔主要な業績〕Monitoring rapid head scarp movement in an alpine rockslide
R. Nishii; N. Matsuoka
ENGINEERING GEOLOGY, 2010年09月, ［査読有り］ - 〔主要な業績〕Solifluction and mudflow on a limestone periglacial slope in the Swiss Alps: 14 years of monitoring
Matsuoka; N, 筆頭著者, Wiley
Permafrost and Periglacial Processes, 2010年09月, ［査読有り］ - Dynamics of solifluction lobes in the Swiss Alps: A summary of 14-year monitoring.
Matsuoka, N, European Geoscience Union
Geophysical Research Abstracts, 2009年04月 - 〔主要な業績〕Permafrost and climate in Europe: Monitoring and modelling thermal, geomorphological and geotechnical responses
Charles Harris; Lukas U. Arenson; Hanne H. Christiansen; Bernd Etzelmuller; Regula Frauenfelder; Stephan Gruber; Wilfried Haeberli; Christian Hauck; Martin Hoelzle; Ole Humlum; Ketil Isaksen; Andreas Kaab; Martina A. Kern-Luetschg; Michael Lehning; Norikazu Matsuoka; Julian B. Murton; Jeanette Noezli; Marcia Phillips; Neil Ross; Matti Seppala; Sarah M. Springman; Daniel Vonder Muehll
EARTH-SCIENCE REVIEWS, 2009年02月, ［査読有り］ - 〔主要な業績〕Permafrost and hydrology in the source area of the Yellow River
松岡; 憲知; 池田; 敦; 末吉; 哲雄, 筆頭著者, チベット高原北東部に位置する黄河源流域において，永久凍土分布とその縮小を明らかにするために，2003年から2006年にかけて凍土環境の調査を行った．まず標高3250 ～4800 m間の18 ヵ所において，弾性波探査，電気探査と地温調査により永久凍土の有無を調べ，GISを用いて探査結果に最も合う永久凍土分布図を作成した．また，マドォ測候所（標高4273 m）にて2年間，気温，地温（0 ～8 m深），降水量，積雪深，土壌水分，地下水位の連続観測を行い，地中の熱および水文条件の季節変化について検討した．さらに，地温プロファイルの数値シミュレーションによって，観測されている気温変化（温暖化）によって，永久凍土がどの程度縮小しうるか検討した． 速いP波伝播速度（＞2 km/s）と相対的に高い電気比抵抗値（650 ～1100 Ωm）が地下浅い位置に検出された標高4300 m以上の地点では，厚さ10 ～30 mの永久凍土層があると推定された．一方，標高4000 m以下では堆積物全体が遅いP波速度（＜1 km/s）を示し，永久凍土は存在しないと考えられる．標高4200 ～4300 mにある広大な沖積低地では，永久凍土は存在しないか，かなり縮小していた．年平均地表面温度（MAST）が負値となるのも4300 m以上で，その標高以上にのみ永久凍土が広範に分布すると予想された．測候所では季節的な凍結が深さ2.6 mまで及んだ．冬季，積雪をほとんど欠くことが，厚い季節凍土層が形成される主因だろう．1980年代の文献には，測候所の地下に永久凍土が存在するとされていたが，深さ4 ～8 mの地温は2年間にわたり0°Cを上回っていた（＜4 °C）．MASTの年々変化が年平均気温の変化に従うとすると，標高4200 ～4300 mにある沖積低地で過去半世紀以内に，永久凍土が急激に縮小したと考えられる．数値シミュレーションからも，薄い（＜15 m）永久凍土層であればその期間内に急激に縮小しうることが示された．近年の温暖化は，源流域において約3000 km2 に及ぶ沖積低地の永久凍土を縮小させていると推定された., 産業技術総合研究所地質調査総合センター
地質調査研究報告, 2009年01月 - 〔主要な業績〕Frost weathering and rockwall erosion in the southeastern Swiss Alps: Long-term (1994-2006) observations
Norikazu Matsuoka, 筆頭著者
GEOMORPHOLOGY, 2008年07月, ［査読有り］ - Thermal history of degrading permafrost in the source region of Yellow River, northeastern Tibet
Sueyoshi; T; Ikeda; A; Matsuoka; N; Ishii; T, Institute of Northern Engineering, University of Alaska
Ninth International Conference on Permafrost, 2008年06月, ［査読有り］ - 〔主要な業績〕Ice-wedge polygon dynamics in Svalbard: High resolution monitoring by multiple techniques
Matsuoka; N; Christiansen; HH, 筆頭著者, University of Alaska Fairbanks
Proceedings of 9th International Conference on Permafrost, 2008年06月, ［査読有り］ - Sounding ice and soil wedge structures with ground-penetrating radar
Watanabe; T; Matsuoka; N; Christiansen; H H; Ikeda; A, Institute of Northern Engineering, University of Alaska
Ninth International Conference on Permafrost, 2008年06月, ［査読有り］ - 〔主要な業績〕Frost weathering: Recent advances and future directions
Norikazu Matsuoka; Julian Murton, 筆頭著者
PERMAFROST AND PERIGLACIAL PROCESSES, 2008年04月, ［査読有り］, ［招待有り］ - 〔主要な業績〕Fast deformation of perennially frozen debris in a warm rock glacier in the Swiss Alps: An effect of liquid water
Atsushi Ikeda; Norikazu Matsuoka; Andreas Kaab
JOURNAL OF GEOPHYSICAL RESEARCH-EARTH SURFACE, 2008年03月, ［査読有り］ - 〔主要な業績〕Involutions resulting from annual freeze-thaw cycles: a laboratory simulation based on observations in northeastern Japan
Yoshiko Ogino; Norikazu Matsuoka, 責任著者
PERMAFROST AND PERIGLACIAL PROCESSES, 2007年10月, ［査読有り］ - Permafrost Sounding (2003-2005) in the Source Area of the Yellow River, Northeastern Tibet
IKEDA Atsushi; SUEYOSHI Tetsuo; MATSUOKA Norikazu; ISHII Takemasa; UCHIDA Youhei, Present-day distribution and ongoing degradation of permafrost were evaluated by geophysical means in the source area of the Yellow River, located at the northeastern margin of the Tibetan Plateau. Seismic, electrical and/or thermal soundings were undertaken at 15 sites between 3260m and 4790m ASL in 2003-2005. High P-wave velocities (>2kms-1) and relatively high DC resistivities (650-1100Ωm) below a thin uppermost layer show that permafrost 10-30m in thickness occurs above 4300m ASL. In contrast, low P-wave velocities (<1kms-1) throughout the uppermost ten to fifteen meters of sediments indicate that permafrost is absent below 4000m ASL. On widespread alluvial plains between 4200m and 4300m ASL, some sites show subsurface intermediate P-wave velocities (1.5-1.7kms-1) and low resistivities (30-140Ωm) indicating the presence of unfrozen-saturated sediments, while others show high DC resistivities possibly indicating the presence of permafrost. Negative values of the mean annual ground surface temperature (MAST) also indicate widespread permafrost only above 4300m ASL under the present climatic condition. Assuming that the inter-annual variation in MAST follows that in the mean annual air temperature, permafrost is estimated to have significantly thawed on the alluvial plains at 4200-4300m ASL during the last half-century., The Association of Japanese Geographers
地理学評論, 2007年 - 〔主要な業績〕Quaternary bedrock erosion and landscape evolution in the Sor Rondane Mountains, East Antarctica: Reevaluating rates and processes
Norikazu Matsuoka; Celine E. Thomachot; Chiaki T. Oguchi; Tamao Hatta; Masahiro Abe; Hiroyuki Matsuzaki, 筆頭著者
GEOMORPHOLOGY, 2006年11月, ［査読有り］ - 〔主要な業績〕Riverbank freeze-thaw erosion along a small mountain stream, Nikko volcanic area, central Japan
Manabu Yumoto; Takayuki Ogata; Norikazu Matsuoka; Eiji Matsumoto
PERMAFROST AND PERIGLACIAL PROCESSES, 2006年10月, ［査読有り］ - 〔主要な業績〕High-centered polygons in the So/r Rondane Mountains, East Antarctica: Possible effect of ice wedge sublimation
Matsuoka; Norikazu; Hirakawa; Kazuomi, 筆頭著者, Small high-centered polygons, 3-15m in diameter, dominate moraine fields in an inland cold desert of the Sr Rondane Mountains, Antarctica. They mainly occur on moraine fields at two stages younger than 1Ma. The polygons on the younger moraine (<0.5Ma) generally have an ice wedge surrounded by ice-cemented permafrost, although the ice wedge cracking is inactive or too slow to be detectable. The polygons on the older moraine (0.5-1Ma) have either an ice wedge or ice-free wedge. The ice-free wedge underlies a subsided trough and consists entirely of loose and coarse sediments with vertically-oriented clasts, which represents an ice-wedge cast probably originating from long-term sublimation of an ice wedge. These observations suggest that flat-top polygons with ice wedges form in wet permafrost when located close to the ice sheet surface, but that the subsequent ice sheet lowering separates the polygons from the moisture source, and finally long-term ice sublimation leads to domed polygons with ice-wedge casts enclosed in dry permafrost., 国立極地研究所
Polar geoscience, 2006年10月, ［査読有り］ - 〔主要な業績〕Monitoring periglacial processes: Towards construction of a global network
Norikazu Matsuoka
GEOMORPHOLOGY, 2006年10月, ［査読有り］ - 〔主要な業績〕Permafrost creep and rock glacier dynamics
Wilfried Haeberli; Bernard Hallet; Lukas Arenson; Roger Elconin; Ole Humlun; Andreas Kaab; Viktor Kaufmann; Branko Ladanyi; Norikazu Matsuoka; Sarah Springman; Daniel Vonder Muhll
PERMAFROST AND PERIGLACIAL PROCESSES, 2006年07月, ［査読有り］ - Comparison of geophysical investigations for detection of massive ground ice (pingo ice)
K Yoshikawa; C Leuschen; A Ikeda; K Harada; P Gogineni; P Hoekstra; L Hinzman; Y Sawada; N Matsuoka
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2006年06月, ［査読有り］ - 〔主要な業績〕Pebbly versus bouldery rock glaciers: Morphology, structure and processes
A Ikeda; N Matsuoka
GEOMORPHOLOGY, 2006年02月, ［査読有り］ - 〔主要な業績〕Temporal and spatial variations in periglacial soil movements on alpine crest slopes
N Matsuoka
EARTH SURFACE PROCESSES AND LANDFORMS, 2005年01月, ［査読有り］ - 〔主要な業績〕Morphometric analysis of solifluction lobes and rock glaciers in the Swiss Alps
N Matsuoka; A Ikeda; T Date, 筆頭著者
PERMAFROST AND PERIGLACIAL PROCESSES, 2005年01月, ［査読有り］ - 〔主要な業績〕Frost damage of bricks composing a railway tunnel monument in Central Japan: field monitoring and laboratory simulation
C Thomachot; N Matsuoka; N Kuchitsu; M Morii
NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2005年, ［査読有り］ - Permafrost sounding (2003-2004) in the source area of the Yellow River, China
Matsuoka; N; Ikeda; A; Sueyoshi; T; Ishii; T
Annual Report of the Institute of Geoscience, the University of Tsukuba, 2004年12月 - 黄河源流域における永久凍土探査(予報)
池田; 敦; 松岡; 憲知; 末吉; 哲雄, 日本雪氷学会
雪氷, 2004年03月, ［査読有り］ - 〔主要な業績〕Present-day periglacial environments in central Spitsbergen, Svalbard
Matsuoka; N; Sawaguchi; S; Yoshikawa; K, 筆頭著者
Geographical Review of Japan, 2004年01月, ［査読有り］ - 〔主要な業績〕Monitoring periglacial processes: New methodology and technology
N Matsuoka; O Humlum, 筆頭著者
PERMAFROST AND PERIGLACIAL PROCESSES, 2003年10月 - 〔主要な業績〕Mountain permafrost in Japan: distribution, landforms and thermal regimes
M Ishikawa; K Fukui; M Aoyama; A Ikeda; Y Sawada; N Matsuoka
ZEITSCHRIFT FUR GEOMORPHOLOGIE, 2003年03月 - A rapidly moving small rock glacier at the lower limit of the mountain permafrost belt in the Swiss Alps
A Ikeda; N Matsuoka; A Kaab
PERMAFROST, VOLS 1 AND 2, 2003年, ［査読有り］ - 〔主要な業績〕Contemporary periglacial processes in the Swiss Alps: seasonal, inter-annual and long-term variations
N Matsuoka; A Ikeda; K Hirakawa; T Watanabe
PERMAFROST, VOLS 1 AND 2, 2003年, ［査読有り］ - 〔主要な業績〕Contemporary permafrost and periglaciation in Asian high mountains: an overview
Matsuoka; N
Zeitschrift fur Geomorphologie, Supplement Band, 2003年01月, ［査読有り］ - 〔主要な業績〕Differential frost heave and sorted patterned ground: field measurements and a laboratory experiment
Matsuoka; N; Abe; M; Ijiri; M, 筆頭著者
Geomorphology, 2003年01月, ［査読有り］ - 〔主要な業績〕アジアの山岳永久凍土と周氷河環境
松岡; 憲知, Asian high mountains involve a large area and a wide variety of periglacial environments. This paper reviews distribution, landscapes and geomorphic processes of mountain permafrost and periglacial belts in the Asian mountains. The lower limit of mountain permafrost descends northwards at a rate of about 160 m per degree of latitude. At the same latitudes, arid continental mountains have a lower limit about 1, 000 m higher than humid mountains, which contrasts with the subpolar mountain permafrost in Scandinavia. The altitudinal extent of the mountain permafrost belt commonly exceeds 700 m in the arid continental mountains, while it is generally less than 700 m in the humid continental and Pacific mountains. A non-permafrost but deep seasonal frost area usually lies between the lower limit of permafrost and the timberline. In the arid continental mountains, despite a vast extent of the periglacial environments, the lack of moisture minimizes frost action that produces typical periglacial landforms. However, the large height of the permafrost belt, when combined with local moisture sources, can produce very long rock glaciers and block streams. In the humid Himalaya, steep rockwalls, 社団法人 東京地学協会
地學雜誌, 2002年08月, ［査読有り］ - 〔主要な業績〕Degradation of talus-derived rock glaciers in the upper engadin, Swiss alps
Atsushi Ikeda; Norikazu Matsuoka
Permafrost and Periglacial Processes, 2002年, ［査読有り］ - 〔主要な業績〕Rock slope failures associated with deglaciation: some examples from glaciated valleys in the Swiss Alps
Matsuoka; N; Abe; M
Annual Report of the Institute of Geoscience, the University of Tsukuba, 2002年01月 - 〔主要な業績〕Weathering in cold regions: Some thoughts and perspective
Kevin Hall; Colin E. Thorn; Norikazu Matsuoka; Angelique Prick
Progress in Physical Geography, 2002年, ［査読有り］ - 〔主要な業績〕Microgelivation versus macrogelivation: towards bridging the gap between laboratory and field frost weathering
Matsuoka; N
Permafrost and Periglacial Processes, 2001年01月, ［査読有り］ - 〔主要な業績〕Direct observation of frost wedging in alpine bedrock
Matsuoka; N
Earth Surface Processes and Landforms, 2001年01月, ［査読有り］ - 〔主要な業績〕Geological controls on the distribution of talus-derived rock glaciers
Matsuoka; N; Ikeda; A
Annual Report of the Institute of Geoscience, the University of Tsukuba, 2001年01月 - 〔主要な業績〕Solifluction rates, processes and landforms: A global review
Norikazu Matsuoka
Earth-Science Reviews, 2001年, ［査読有り］ - 欧州アルプス山岳永久凍土帯の斜面変動
松岡; 憲知; 平川; 一臣; 渡辺; 悌ニ; 池田; 敦, 社団法人 東京地学協会
地學雜誌, 2000年10月 - 〔主要な業績〕Solifluction resulting from one-sided and two-sided freezing : Field data from Svalbard.
Matsuoka; N; Hirakawa; K
Polar Geoscience, 2000年01月, ［査読有り］ - 〔主要な業績〕Controls on sorted patterned-ground geometry in the Swiss Alps
Abe; M; Matsuoka; N
Annual Report of the Institute of Geoscience, the University of Tsukuba, 2000年01月 - 〔主要な業績〕Monitoring of thermal contraction cracking at an ice wedge site, central Spitsbergen.
Matsuoka; N
Polar Geoscience, 1999年01月, ［査読有り］ - 〔主要な業績〕Measurements of bottom temperature of the winter snow cover (BTS) in relation to rock glacier activity, Corviglia, Swiss Alps : a preliminary report. (共著)
Ikeda; A; Matsuoka; N
Annual Report of the Institute of Geoscience, the University of Tsukuba, 1999年01月 - 〔主要な業績〕Rockfall activity from an alpine cliff during thawing periods (共著)
Matsuoka; N; Sakai; H, 筆頭著者
Geomorphology, 1999年01月, ［査読有り］ - 〔主要な業績〕Modelling frost creep rates in an alpine environment
Matsuoka; N
Permafrost and Periglacial Processes, 1998年11月, ［査読有り］ - 〔主要な業績〕The role of diurnal, annual and millennial freeze-thaw cycles in controlling alpine slope stability(共著)
Matsuoka; N; Hirakawa; K; Watanabe; T; Haeberli; W; Keller; F, 筆頭著者, Centre d'etudes nordiques, Universite Laval
Proceedings of the Seventh International Conference on Permafrost, 1998年07月, ［査読有り］ - 〔主要な業績〕Some observations regarding mountain permafrost in the Japanese Alps(共著)
Matsuoka; N, 筑波大学
Annual Report of the Institute of Geoscience, the University of Tsukuba, 1998年01月 - Monitoring rockwall instability in the Murt(]E85C2[)l-Corvatsch region, Upper Engadin
Matsuoka; N
Beitr(]E88D2[)ge aus der Gebirgs-Geomorphologie, Mitteilungen der Versuchsanstalt f(]E88DB[)r Wasserbau, Hydrologie und Glaziologie der Eidgen(]E88D8[)ssischen Technischen Hochschule Z(]E88DB[)rich, 1998年01月, ［査読有り］ - 〔主要な業績〕The relationship between frost heave and downslope soil movement : field measurements in the Japanese Alps
Matsuoka; N
Permfrost and Periglacial Processes, 1998年01月, ［査読有り］ - 〔主要な業績〕岩石氷河－氷河説と周氷河説－
松岡憲知, Recent progress in rock glacier studies is reviewed with some emphases on the competition between the glacial and periglacial hypotheses. Rock glaciers are tongue-shaped or lobate bodies composed of angular boulders that resembles a small glacier, usually accompanied by multiple transverse ridges resulting from a compressive flow. Rock glaciers are classified, in terms of the origin of surface materials, into talus and morainic rock glaciers, and in the light of the activity status, into active, inactive and fossil ones. The distribution of active rock glaciers are delimited by the regional glacier equilibrium line and lower limit of mountain permafrost.
The internal structure of rock glaciers has been approached by direct observations and indirect geophysical soundings. In some rock glaciers, natural outcrops exhibit a massive ice body with debris bands beneath the surface boulder layer, which has encouraged the glacial hypothesis. Massive ice was also found in boreholes penetrating through a rock glacier permafrost in the Swiss Alps, despite being considered to originate from snow avalanche or refrozen meltwater. In fact, deformation occurred mostly in the frozen debris layer beneath the massive ice, indicating the periglacial origin of the rock glacier due to permafrost creep. Geophysical soundings, including seismic, geoelectric and gravimetric measurements, have provided useful information on the three-dimensional structure, stratigraphy and ice contents of rock glacier bodies, although authors preferring the glacial hypothesis tend to reject such indirect results. The origin of any rock glacier is thus equivocal without detailed analyses of internal stratigraphy and ice composition.
Most of the active rock glaciers are moving at a speed of 101 cm yr-1, two orders of magnitude slower than 'ice' glaciers. The periglacial model attributes such a slow movement to permafrost creep. A possible consequence of this is that active rock glaciers usually have ages of several thousand years ; that inactive ones were activated repeatedly during the colder periods of the Holocene; and that fossil ones moved during the Late Glacial. In contrast, the glacial model explains that many rock glaciers originated from a debris-covered glacier during the Little Ice Age and have been loosing their ice content and speed rapidly with the 20th-Century warming.
Only a few rock glaciers have been identified from Japanese mountains. Although locations favorable for active rock glaciers are restricted to the northern side of some high mountains, the mountain permafrost belt must have been wide enough to form a number of rock glaciers during some past cold periods. Subsequent permafrost melting would have fossilized these rock glaciers, some of which may have been misinterpreted as glacial moraines or protalus ramparts., 東京地学協会
地学雑誌, 1998年01月, ［査読有り］ - 〔主要な業績〕Monitoring of periglacial slope processes in the Swiss Alps : the first two years of frost shattering, heave and creep(共著)
Matsuoka, N; Hirakawa, K; Watanabe, T; Moriwaki, K, 筆頭著者, John Wiley and Sons Ltd
Permafrost and Periglacial Processes, 1997年, ［査読有り］ - 〔主要な業績〕Soil moistrure variability in relation to diurnal frost heaving on Japanese high mountain slopes
Matsuoka; N
Permafrost and Periglacial Processes, 1996年01月, ［査読有り］ - 〔主要な業績〕Field experiments on physical weathering and wind erosion in an Antarctic cold desert(共著)
Matsuoka, N; Moriwaki, K; Hirakawa, K, John Wiley and Sons Ltd
Earth Surface Processes and Landforms, 1996年, ［査読有り］ - 〔主要な業績〕The effect of rock properties on rates of tafoni growth in coastal environments(共著)
Matsukura; Y; Matsuoka; N
Zeitschrift f(]J1168[)r Geomorphologie, Supplement Band, 1996年01月, ［査読有り］ - 〔主要な業績〕Rock weathering processes and landform development in the Sør Rondane Mountains, Antarctica
Norikazu Matsuoka
Geomorphology, 1995年, ［査読有り］ - 〔主要な業績〕A laboratory simulation on freezing expansion of a fractured rock : preliminary data
Matsuoka; N, 筑波大学
Annual Report of the Institute of Geoscience, the University of Tsukuba, 1995年01月 - 〔主要な業績〕Continuous recording of frost heave and creep on a Japanese alpine slope
Matsuoka; N
Arctic and Alpine Research, 1994年01月, ［査読有り］ - 〔主要な業績〕Diurnal freeze–thaw depth in rockwalls: Field measurements and theoretical considerations
Norikazu Matsuoka
Earth Surface Processes and Landforms, 1994年, ［査読有り］ - Monitoring system for some periglacial processes
Matsuoka; N
Annual Report of the Institute of Geoscience, the University of Tsukuba, 1993年01月 - 〔主要な業績〕Critical polygon size for ice-wedge formation in Svalbard and Antarctica (共著)
Matsuoka; N; Hirakawa; K
Proceedings of the Sixth International Conference on Permafrost, 1993年01月, ［査読有り］ - 〔主要な業績〕凍結融解作用の機構からみた周氷河地形
松岡; 憲知, 凍結融解作用の物理的機構に基づいて,周氷河地形の形成過程を論ずるうえでの問題点について述べる.地温が0C°直下に達したときに生じる凍結膨張によって,岩石は破砕され,土は凍上する.凍結膨張した地盤が融解するときに,沈下ないし物性の変化を起こすことによって物質が移動し,地形が変化する.その地形変化速度は,凍結融解の頻度,水分条件,地盤の物性など種々の因子に支配される.日周期性と年周期性の凍結融解作用の凍結(融解)深度の違いは,岩壁から落下する礫の粒径や斜面物質の移動限界深度に影響を及ぼす.気候条件(寒さ・湿度・永久凍土の有無など)と凍結融解作用(地形変化速度・変化様式・生成物質など)との関係を議論するたあには,凍結融解作用を支配する個々の因子を定量的に評価する必要がある., 日本地理学会 古今書院(発売)
地理学評論 Ser.A, 1992年02月, ［査読有り］ - 〔主要な業績〕Frost heave and creep in the sor Rondane Mountains, Antarctica (共著)
Matsuoka; N; Moriwaki; K, 筆頭著者
Arctic and Apline Research, 1992年01月, ［査読有り］ - セールロンダーネ山地地学調査隊報告 1990/91(JARE-32)
岩田; 修二; 白石; 和行; 海老名; 頼利; 松岡; 憲知; 豊島; 剛志; 大和田; 正明; 長谷川; 裕彦; Decleir; Hugo; Pattyn; Frank, 第32次南極地域観測隊(JARE-32)夏隊のセールロンダーネ山地地学調査隊は, 1990年12月24日あすか観測拠点を出発し, 1991年2月7日に再び「あすか」に帰り着くまでセールロンダーネ山地中央部で, 地形・地質・雪氷調査を行い測地作業も実施した。雪上車とスノーモービルを利用してキャンプを移動しながら調査するという従来と同じ行動様式をとったため, 設営面でもおおかたはこれまでの方式と同じである。地学調査は, 地形では, 野外実験地の撤収, 岩石の風化の調査, モレーン・ティルのマッピング, 地質では, 構成岩石の形成順序の解明, 構造地質学的・構造岩石学的そして地球化学的研究のためのサンプリング, 測地では, 重力測量, 地磁気測量, GPSによる基準点測量が行われた。ベルギーからの交換科学者は氷河流動・氷厚などを測定した。, 国立極地研究所
南極資料, 1991年11月 - 〔主要な業績〕年平均気温から地盤の最大凍結・融解深度を推定する方法(短報)
松岡; 憲和, A method is described for the prediction of maximum freeze/thaw penetration depth in snow-and vegetation-free ground as a function of the mean annual air temperature. Annual variation in ground surface temperature was fitted by a sinusoidal curve with the amplitude, Tos. The meteorological data show that the value of Tos ranges from 11° to 16°C in Japan. Three sinusoidal curves with the Tos values of 11°, 13° and 15°C were used for the calculation of the freeze/thaw depth. The Aldrich equation allowed the calculation to be made. The freezing and thawing indices involved in this equation were determined for every degree of the mean annual ground surface temperature. The maximum freeze/thaw depth was calculated for four kinds of ground materials, i.e., volcanic ash, sand/silt, gravel and rock, and then plotted against the mean annual surface temperature. The diagram indicates that the freeze/thaw depth increases as mean annual surface temperature approaches 0°C and with rising both thermal conductivity and volumetric water content of the ground material.
The relationship between the mean annual air temperature and the maximum freeze/thaw depth was obtained using the empirical relation between the mean ground surface and air temperatures. The predicted depths agreed fairly well with the measured depths in various cold environments where the mean annual air temperature is known., 日本地理学会 古今書院(発売)
地理学評論 Ser.A, A, 1991年05月, ［査読有り］ - 〔主要な業績〕A model of the rate of frost shattering: Application to field data from Japan, Svalbard and Antarctica
Norikazu Matsuoka
Permafrost and Periglacial Processes, 1991年, ［査読有り］ - 〔主要な業績〕Ground temperature regimes and their relation to periglacial processes in the Sφr Rondane Mountains, East Antarctica (共著)
Matsuoka; N; Moriwaki; K; Iwata; S; Hirakawa; K
Proceedings of the NIPR Symposium on Antarctic Geosciences, 1990年01月, ［査読有り］ - 〔主要な業績〕Mechanisms of rock breakdown by frost action: An experimental approach
Norikazu Matsuoka
Cold Regions Science and Technology, 1990年, ［査読有り］ - 〔主要な業績〕The rate of bedrock weathering by frost action: Field measurements and a predictive model
Norikazu Matsuoka
Earth Surface Processes and Landforms, 1990年, ［査読有り］ - 〔主要な業績〕Diurnal forst-heave activity in the Sφr-Rondane Mountains, Antarctica (共著)
Matsuoka; N; Moriwaki; K; Hirakawa; K
Arctic and Alpine Research, 1988年01月, ［査読有り］ - 〔主要な業績〕Laboratory experiments on frost shattering of rocks
Matsuoka; N, 筑波大学
Science Report of the Institute of Geoscience, University of Tsukuba, Sect. A, 1988年01月, ［査読有り］ - セールロンダーネ山地地学調査隊報告1987(JARE-28)
平川; 一臣; 松岡; 憲知; 高橋; 裕平; 先山; 徹; 小山内; 康人; 田中; 幸生, 第28次南極地域観測隊のセールロンダーネ山地地学調査は, 山地中央部において, 1月7日から2月10日にかけて実施された。調査はJARE-26,-27の調査地域内に限定し, 精査を旨とした。スノーモービルの活用と天候に恵まれ, ほぼ予定どおりの調査を行うことができた。この報告では, 主として行動とその問題点について記載するとともに行動中の気象表を提示する。地学調査の成果については別途に詳しく報告することとし, 概略を記すにとどめる。なお, 今次行動にはベルギー国から2人の地球科学者が交換科学者として参加し, 氷河地形学的調査を行った。, 国立極地研究所
南極資料, 1987年11月 - セールロンダーネ山地地学調査隊報告1986(JARE-27)
森脇; 喜一; 小島; 秀康; 石塚; 英男; 松岡; 憲知; 米渓; 武次; 志賀; 重男; 森田; 知弥; 栗城; 繁夫, 第27次南極地域観測隊のセールロンダーネ山地地学調査は, 山地中央部地域において, あすか観測拠点の発電棟建設作業終了後, 1月5日から2月6日にかけて実施された。現在は山地の概査を行っている期間であり, 広域を対象とするため調査は2班に分かれて実施した。数多くのクレバスがあって調査活動は必ずしも容易ではなかったが, 2月の天候不順が懸念されたので, 早めに日程を消化するよう努めた。調査予定地域のほぼ全域を調査できたが, これはスノーモービルを十分に活用できたことによるところが大きい。ここでは設営面を含めた行動の概要とその問題点を中心に記述する。また, 今後の調査行動に資するため, 気象・雪氷状況を主として図表によりやや詳しく報告する。地学調査の成果については, 現在, 整理研究中であるので, 野外調査の概略を記すにとどめる。, 国立極地研究所
南極資料, 1986年11月 - 〔主要な業績〕ネパール・ヒマラヤの氷河周辺における岩盤の凍結破砕作用について
松岡; 憲知, ネパール・ヒマラヤにおける通年の気象記録をもとに, 氷河周辺での岩盤の凍結破砕作用の強さについて推定した.標高4000m以上では年間150回以上に及ぶ凍結融解の繰り返しが起こる.とくに標高5000~5500mに露出する岩盤では, 凍結融解の発生期がモンスーン季に一致するため, 凍結破砕の発生に必要な水分の供給が豊富である.この高頻度の凍結融解の繰り返しと豊富な水分の存在下で, 強力な凍結破砕作用が働き, 氷河上へ多量の岩屑が供給されていると考えられる., 社団法人 日本雪氷学会
雪氷, 1984年01月, ［査読有り］
MISC
- マラソンコースを地形学で読み解く
松岡憲知
月刊地理, 2020年08月, ［招待有り］ - 第1回ヨーロッパ永久凍土会議 (イタリア・ローマ) に参加して
松岡 憲知; 曽根 敏雄; 石川 守; 澤田 結基; 福井 幸太郎; 池田 敦
地形 = Transactions, Japanese Geomorphological Union, 2001年04月25日 - The Periglaciation of Great Britain/Colin K.Ballantyne and Charles Harris(1994)
松岡 憲知
地理学評論 Ser.A A, 1995年09月 - WEATHERING STAGE OF TILL AND GLACIAL HISTORY OF THE CENTRAL SOR RONDANE MOUNTAINS, EAST ANTARCTICA
MORIWAKI Kiichi; HIRAKAWA Kazuomi; MATSUOKA Norikazu
Proceedings of the NIPR Symposium on Antarctic Geosciences, 1991年09月 - A preliminary study on tafoni and honeycombs in Nojimazaki, Boso Peninsula, Japan
Matsukura Yukinori; Matsuoka Norikazu; Yano Noriko
Annual report of the Institute of Geoscience, the University of Tsukuba, 1989年 - RECONSTRUCTION OF MAXIMUM GLACIAL EXTENT IN THE CENTRAL S∅R RONDANE MOUNTAINS, EAST ANTARCTICA
HIRAKAWA Kazuomi; MATSUOKA Norikazu; MORIWAKI Kiichi
Proceedings of the NIPR Symposium on Antarctic Geosciences, 1988年09月
書籍等出版物
- 〔主要な業績〕地形の辞典
松岡憲知, 分担執筆
朝倉書店, 2017年02月
9784254160635 - Field guide for excursions, EUCOP III Svalbard, Norway 13-18 June 2010
Christiansen; HH; Matsuoka; N; Watanabe; T, 分担執筆
Geological Survey of Norway, 2010年06月 - 北極圏の周氷河環境を探る
松岡憲知, 単著
極地 86, 2008年01月 - 〔主要な業績〕地球環境学
松岡憲知; 田中; 博; 杉田倫明; 村山祐司; 手塚 章; 恩田裕一; 松岡; 憲知, 編者(編著者)
古今書院, 2007年04月
9784772252034 - Dilation of building materials submitted to frost action
Thomachot; CE; Matsuoka; N, 共著
Building Stone Decay: From Diagnosis to Conservation, Geological Society of London, 2007年01月, ［査読有り］
9781862392182 - 〔主要な業績〕Solifluction (Encycropedia of Geomorphology 2)
Matsuoka; N, 分担執筆
Goudie, A.S. (ed.) Encycropedia of Geomorphology 2, Routledge, 2004年01月, ［査読有り］
9780415863001
講演・口頭発表等
- 〔主要な業績〕スイスの山と日本の山 ーＵとＶが生み出す自然環境・人間生活 ・ ツーリズムの特色を比較するー
松岡憲知
放送大学ライブラリー講演会, 2025年03月22日, ［招待有り］ - 〔主要な業績〕歩いて走って考える地形学－スイスアルプスバーチャル巡検＋マラソンコースを地形学で読み解く－
松岡憲知
日本地形学連合（JGU）地形の学校2024, ［招待有り］
20240928, 20240929 - 〔主要な業績〕How do permafrost landforms in Svalbard respond to global warming?
Norikazu Matsuoka; Tatsuya Watanabe; Hanne H. Christiansen
12th International Conference on Permafrost, 2024年06月19日 - 〔主要な業績〕How large and how fast can needle ice transport stones downslope? Lessons from two-decade observations in the Japanese Alps
Norikazu Matsuoka
6th European Conference on Permafrost, 2023年06月20日 - Periglacial landforms as climatic indicators: What do sorted patterns tell us?
Norikazu Matsuoka
CryoKarst kick-off meeting, 2023年01月23日, ［招待有り］
20230123 - 〔主要な業績〕南アルプスでジオトレイル
松岡憲知
山梨大学地域貢献公開シンポジウム,「やまなしの森の活かし方」, 2021年12月12日, 山梨大学人材養成センター, ［招待有り］
20221212 - 〔主要な業績〕海食凹地形の分類と形成条件
松岡憲知・篠原叶実・伊藤敦哉・牛込佳太・小倉拓郎・小玉芳敬・金山恭子
日本地形学連合2022年秋季大会, 2022年11月06日, 日本地形学連合
20221105, 20221106 - 岩石海岸の海食凹地形におけるロックコントロール
篠原; 叶実; 松岡; 憲知
日本地形学連合2020年秋季大会, 2020年11月29日 - 〔主要な業績〕Decadal dynamics of permafrost landforms in Svalbard
Matsuoka; Norikazu
Sixth International Symposium on Arctic Research, 2020年03月18日, Japan Consortium for Arctic Environmental Research - 〔主要な業績〕Differential frost heave on incipient sorted patterns in the Japanese Alps: a multi-method monitoring
Matsuoka; Norikazu
First Southern Hemisphere Conference on Permafrost, 2019年12月04日 - 〔主要な業績〕Decadal-scale variability of polar rock glacier dynamics: Accelerating due to warming?
Matsuoka; Norikazu; Watanabe; Tatsuya; Ikeda; Atsushi; Christiansen; Hanne H; Humlum; Ole; Rouyet; Line
First Southern Hemisphere Conference on Permafrost, 2019年12月04日 - スピッツベルゲンの岩石氷河の運動にみる年々変動と長期傾向
松岡; 憲知
永久凍土の変動とそのモニタリングに関する研究集会, 2019年11月18日 - 〔主要な業績〕氷楔形成縁辺域における氷楔破壊発生の年々変動－スバルバールでの12年間の観測総括－
松岡; 憲知; 渡邊達也; Hanne; H. Christiansen
日本地球惑星科学連合2018年度連合大会, 2018年05月23日, 日本地球惑星科学連合 - 南アルプスの小型構造土での差別凍上観測（2013～2017）
松岡; 憲知
永久凍土の変動とそのモニタリングに関する研究集会, 2018年03月08日, 国立極地研究所 - Mountain Science Frontiers: Planning International and Interdisciplinary Studies
Matsuoka; Norikazu
International Symposium on Mountain Sciences 2017, 2017年11月15日, 筑波大学山岳科学センター - 〔主要な業績〕A multi-method approach to detecting bedrock fracturing and rockfall activity in the Southern Japanese Alps
Matsuoka; Norikazu
The Fourth Slope Tectonics Conference, 2017年10月14日 - 〔主要な業績〕From needle ice to deep permafrost: Classifying periglacial environments based on prevailing frost action
Matsuoka; Norikazu
2nd Asian Conference on Permafrost, 2017年07月02日, International Permafrost Association, ［招待有り］ - 〔主要な業績〕Multi-method monitoring of ice wedge dynamics in central Spitsbergen (2005-2016)
Matsuoka; Norikazu; Christiansen; Hanne H; Watanabe; Tatsuya
2nd Asian Conference on Permafrost, 2017年07月02日, International Permafrost Association - 山と自然－山岳科学から持続可能な日本を創生する－
松岡憲知; 津田吉晃
第2回全国「山の日」フォーラム, 2017年05月14日 - 山岳科学の創出－山岳地域の諸問題を分野横断で俯瞰する－
松岡憲知; 渡辺悌二; 横山 智
日本地理学会2007年春季学術大会, 2017年03月29日 - スピッツベルゲンにおける永久凍土動態観測10年（2）極地型岩石氷河の運動
松岡憲知; 渡邊達也; 池田 敦; Hanne; H. Christiansen
永久凍土の変動とそのモニタリングに関する研究集会, 2017年01月16日 - スピッツベルゲンにおける永久凍土動態観測10年（1）アイスウェッジの破壊
松岡憲知; Hanne; H. Christiansen; 渡邊達也
低温研共同研究集会「永久凍土の動態解明のための多角的アプローチ」, 2016年11月21日 - 〔主要な業績〕A multi-method approach to detecting high-mountain rockfall activity
Matsuoka; Norikazu
11th International Conference on Permafrost, 2016年06月19日, International Association on Permafrost - 〔主要な業績〕Slow, but steady movement of an Arctic rock glacier: 10 years of movements and thermal conditions
松岡; 憲知
11th International Conference on Permafrost, 2016年06月19日, International Association on Permafrost - 〔主要な業績〕南アルプスにおける落石の発生時期・規模・原因－多様な手法による分析－
松岡; 憲知
日本地球惑星科学連合2016年度連合大会, 2016年05月24日 - 〔主要な業績〕Interannual variability of ice wedge dynamics in Adventdalen, central Spitsbergen
Matsuoka; Norikazu; Christiansen; Hanne; H; Watanabe; Tatsuya
Fourth Europeanl Conference on Permafrost, 2014年06月21日 - 〔主要な業績〕From kinematics to dynamics: significance of field and laboratory approaches to understand periglacial mass movements
Matsuoka; Norikazu
Fourth European Conference on Permafrost, 2014年06月20日, ［招待有り］ - 〔主要な業績〕南アルプス高山域における岩盤破砕・土砂移動の観測
松岡; 憲知; 西井; 稜子; 池田; 敦
日本地球惑星科学連合2012年大会, 2012年05月20日
担当経験のある科目（授業）
- 自然地理学演習
2021年04月 - 現在
茨城大学 - 自然地理学特講
2021年04月 - 現在
茨城大学 - 自然地理学概論
2021年04月 - 現在
茨城大学 - 地域へのアプローチ
2022年04月 - 2023年03月
茨城大学 - 山岳科学野外実験
2017年04月 - 2021年03月
筑波大学 - 山岳科学概論
2017年04月 - 2021年03月
筑波大学 - 極域地形学
2012年04月 - 2021年03月
筑波大学 - 地球環境学
2007年04月 - 2021年03月
筑波大学 - 氷河凍土学
2007年04月 - 2021年03月
筑波大学 - 地球科学のための英語論文の書き方
2003年04月 - 2021年03月
筑波大学 - 世界地誌
1990年04月 - 2021年03月
筑波大学 - 地形学
1989年04月 - 2021年03月
筑波大学 - 地形学野外実験
1988年04月 - 2021年03月
筑波大学 - 地形プロセス学
1995年04月 - 2007年03月
筑波大学 - 永久凍土と周氷河環境
2003年03月 - 2003年04月
スバルバール大学
所属学協会
共同研究・競争的資金等の研究課題
- 地質条件に基づく伊豆半島の海食地形の分類と形成条件の体系化
2020年 - 2021年 - 周氷河気候指標の高精度化と国際標準の策定
基盤研究(B)
筑波大学
2008年 - 2010年 - 北極圏地球環境科学野外教育コースの設立
萌芽研究
筑波大学
2007年 - 2008年 - 地球規模観測網に基づく周氷河地形変動のモデル化
基盤研究(B)
筑波大学
2005年 - 2007年 - 永久凍土環境と季節凍土環境における周氷河地形形成作用の比較研究
基盤研究(C)
筑波大学
2003年 - 2004年 - 岩石氷河への岩屑の供給機構
筑波大学
2000年 - 2001年 - 中部山岳地域における永久凍土の分布と地形変動
基盤研究(C)
筑波大学
1996年 - 1997年 - 岩壁の凍結破壊と落石の発生機構
一般研究(C)
1994年 - 1995年 - 北極圏スバルバール諸島の周氷河地形
1988年 - 1992年
