309 research outputs found
Depth of the 660-km discontinuity near the Mariana slab from an array of ocean bottom seismographs,
[1] High frequency records of deep Mariana earthquakes from a dense array of ocean bottom seismographs deployed in the Mariana arc and back-arc regions are stacked and searched for the phases P660p and S660p to constrain the depth of the 660-km discontinuity near the Mariana slab. Results of the high-resolution study suggest that around 18°N the 660-km discontinuity lies at about 710-730 km (±14 km) depth within or in the vicinity of the slab core. In the region seismicity ceases at 100 km above the base of the transition zone. These findings and similar observations in Tonga argue that factors other than the phase transition at the base of the upper mantle may control the maximum down-dip extent of the deep seismogenic region in the slab
Finite frequency whole mantle P wave tomography: Improvement of subducted slab images
We present a new whole mantle P wave tomographic model GAP_P4. We used two data groups; short-period data of more than 10 million picked-up onset times and long-period data of more than 20 thousand differential travel times measured by waveform cross-correlation. Finite frequency kernels were calculated at the corresponding frequency bands for both long- and short- period data. With respect to an earlier model GAP_P2, we find important improvements especially in the transition zone and uppermost lower mantle beneath the South China Sea and the southern Philippine Sea owing to broadband ocean bottom seismometers (BBOBS) deployed in the western Pacific Ocean where station coverage is poor. This new model is different from a model in which the full data set is interpreted with classical ray theory. BBOBS observations should be more useful to sharpen images of subducted slabs than expected from simple ray path coverage arguments
Zooplankton communities at the sea surface of the eastern Indian sector of the Southern Ocean during the austral summer of 2018/2019
Knowledge on the distribution of zooplankton in the many unique habitats of the Southern Ocean is essential for understanding food web dynamics, assessing the impacts of environmental change and for managing the exploitation of marine living resources. Variation in the distribution of zooplankton may occur in the horizontal as well as the vertical plane, and the latter may show a diel cycle (diel vertical migration or DVM). Conventional sampling methods, including several types of nets and acoustics, often undersample or ignore the top 10 m of the water column. The surface waters may, however, host a specific zooplankton community and therefore be an important foraging ground for higher trophic level predators. In order to investigate the importance of the surface waters for understanding the distribution of species and potentially improving abundance estimates, the upper two meters of the water column were sampled in the eastern Indian sector of the Southern Ocean using a Surface and Under Ice Trawl (SUIT). Findings were compared to the zooplankton community structure in the epipelagic (15–200 m). Results showed that the surface zooplankton community could largely be divided into two regions. The surface community of the western side of the sampling area hosted large numbers of Antarctic krill, Euphausia superba, which were only present in low densities in the epipelagic depth layer. Densities of Limacina helicina were also relatively high in the west. The copepod Calanus propinquus and the amphipod Themisto gaudichaudii were present in relatively large numbers throughout the sampling area. T. gaudichaudii was the dominant species of the surface in the eastern side of the sampling area in the absence of Antarctic krill. Apart from cirripedia nauplii, no species were uniquely found in the surface water compared to the 15–200 m depth layer. Surface water sampling revealed patterns in vertical distribution and DVM, and showed that these patterns changed between the first and second half of the expedition. This could partially be explained by environmental variables but was likely also a result of sampling time and location, and associated variation in the size and ontogeny of species. Results revealed the impact of undersampling the surface layer regarding knowledge on distribution and vertical migration patterns of zooplankton species
TIARES Project -Tomographic investigation by seafloor array experiment for the Society hotspot
http://www.godac.jamstec.go.jp/darwin/cruise/mirai/mr08-06_leg1/
Cruise Report of JAMSTEC R/V Natsushima NT0801
調査海域: 相模湾 / Area: Sagami Bay ; 期間: 2008年1月7日~2008年1月10日 / Operation Period: January 7, 2008~January 10, 2008http://www.godac.jamstec.go.jp/darwin/cruise/natsushima/nt08-01/
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