Structure of Meridional Circulation in Southern Ocean captured by long term Mooring

The Tenth Symposium on Polar Science/Ordinary sessions: [OM] Polar Meteorology and Glaciology, Wed. 4 Dec. / Entrance Hall (1st floor) , National Institute of Polar Researc

Seasonal variations of sea ice and ocean circulation in the Bering Sea: A model‐data fusion study

Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/94775/1/jgrc11005.pd

Rapid and persistent freshening of Antarctic Bottom Water in the Australian-Antarctic Basin

第6回極域科学シンポジウム分野横断セッション：[IG] 全球環境変動を駆動する南大洋・南極氷床11月17日（火）　国立極地研究所 2階 大会議

100m疾走の後半における走スピード, ピッチおよびストライドの変化

本研究では, 成人男子7名を被験者にして, 100m疾走中の後半における走スピード, ピッチ数およびストライド長の変化を明らかにした。本研究で得られた結果は, 次のように要約できる。1) 100m疾走後半の50mから100mまで, 走スピードは減少し続けた。2) 100m疾走後半の50mから100mまで, ピッチ数は減少し続けた。3) 100m疾走後半の50mから90mまでストライド長はほぼ一定を保ったが, 90mから100mまでの区間ではストライド長は急激に増加した。The purpose of this study was to measure running speed, stride length and step frequecny in the latter half of 100m sprint running. The subjects used in this study were four collegiate jumpers, 2 graduate students and an assistant of Chukyo University. All were healthy males. Each run was filmed at 50 frames/sec with Photosonics and Bolex 16mm cameras. Stride length and step frequency was measured from film analysis. Resultes obtanied from this study were summarized as follows. 1. Running speed and step frquency were gradually decreased in the latter half 50m of 100m sprint running. 2. Stride length was almost constant from 50m to 90m. After that, however, it was significantly decreased

Retrieval of sea-ice thickness distribution in the Sea of Okhotsk from ALOS/PALSAR backscatter data

Although satellite data are useful for obtaining ice-thickness distribution for perennial sea ice or in stable thin-sea-ice areas, they are still largely an unresolved issue for the seasonal ice zone (SIZ). We address this problem using L-band synthetic aperture radar (SAR). In the SIZ, ice-thickness growth is closely related to deformation, so surface roughness is expected to correlate with ice thickness. L-band SAR, suitable for detecting such surface roughness, is a promising tool for obtaining thickness distribution. This idea was supported by an airborne polarimetric and interferometric SAR (Pi-SAR) validation. To extend this result to spaceborne L-band SAR with coarser resolution, we conducted in situ measurements of ice thickness and surface roughness in February 2008 in the southern Sea of Okhotsk with an icebreaker in coordination with the Advanced Land Observing Satellite (ALOS)/Phased Array-type L-band SAR (PALSAR) orbit. A helicopter-borne laser profiler was used to improve the estimation of surface. roughness. It was found that backscatter coefficients (HH) correlated well with ice thickness (R=0.86) and surface roughness (R=0.70), which confirms the possibility of determining ice-thickness distribution in the SIZ. The interannual variation of PALSAR-derived ice-thickness distribution in the southern Sea of Okhotsk is also discussed

Interconnected pores on the walls of a polymeric honeycomb monolith structure created by the unidirectional freezing of a binary polymer solution

Interconnected submicron pores were created on the walls of a honeycomb monolith structure by the unidirectional freezing of a binary polymer solution. Agglomerated globules of polyethylene glycol (PEG) in a binary solution of polystyrene (PS) and PEG in 1, 4-dioxane solvent were frozen unidirectionally in a liquid nitrogen bath. Removing the frozen solvent and the agglomerated globules of PEG by freeze-drying and leaching, respectively, enabled us to create interconnected pores in the PS walls. The combination of PS and PEG was effective in creating interconnected pores in the walls because PS and PEG are poorly soluble in one another. The higher freezing rate and lower PEG weight fraction of the binary solution effectively reduced the pore size in the microtube walls