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81.
Assessing flood disaster impacts in agriculture under climate change in the river basins of Southeast Asia 总被引:1,自引:0,他引:1
Shrestha Badri Bhakta Perera Edangodage Duminda Pradeep Kudo Shun Miyamoto Mamoru Yamazaki Yusuke Kuribayashi Daisuke Sawano Hisaya Sayama Takahiro Magome Jun Hasegawa Akira Ushiyama Tomoki Iwami Yoichi Tokunaga Yoshio 《Natural Hazards》2019,97(1):157-192
Natural Hazards - This study focused on flood damage assessment for future floods under the impact of climate change. Four river basins of Southeast Asia were selected for the study. They included... 相似文献
82.
83.
Current measurements made with a Doppler Current Profiler were taken along cross sections in the Obatake Seto Strait, a small strait in the western part of the Seto Inland Sea.The energy loss between two cross sections of the strait was estimated using the control volume analysis of the stationary one-dimensional energy equation. The large energy loss observed in the strait cannot be explained in terms of general bottom friction in the coastal region. The loss is attributed to the form loss, which is accompanied by internal turbulence and vortices generated by the specific topography of the strait, in addition to the loss by friction. This is supported by the fact that the energy loss in the strait differs, depending upon the current direction. 相似文献
84.
Journal of Oceanography - The water below a depth of 1,000 m in the Japan Sea was found to consist of two water masses, the upper layer (the Deep Water) and the lower layer (the Bottom Water). The... 相似文献
85.
Methane in the western North Pacific 总被引:7,自引:0,他引:7
Shuich Watanabe Naoto Higashitani Nobuo Tsurushima Shizuo Tsunogai 《Journal of Oceanography》1995,51(1):39-60
The concentration of methane in about 400 seawater samples collected in the western North Pacific, mostly from 40°N to 5°S along 165°E was determined. While the concentration of methane in the surface water was slightly greater in the high-latitudes, it did not widely vary with a standard deviation of 0.29 n mol/l for a mean value of 2.49 n mol/l. The 90% confidence limit of the mean was 0.08 n mol/l. The degree of oversaturation in 1991 (31±4%) was not different from that in circa 1970. If we assume that this degree of oversaturation occurs in the entire oceans, the annual flux of methane becomes 6×1012g CH4. Both the concentrations of methane and chlorophylla were higher in the surface 100 m layer. However, the correlation between them was not well in the entire surface waters. This may indicate that the production of methane is not directly related to the photosynthetic process. The concentration of methane decreased gradually with increasing depth down to 1000 m. Its horizontally and vertically uniform concentration in the abyssal water suggests that the turnover time of methane in the oxic pelagic water is in the range between a few years and a few hundred years. 相似文献
86.
Yuji Watanabe Atsushi Yamaguchi Hiroshi Ishida Takashi Harimoto Shinya Suzuki Yoshio Sekido Tsutomu Ikeda Yoshihisa Shirayama Masayuki Mac Takahashi Takashi Ohsumi Joji Ishizaka 《Journal of Oceanography》2006,62(2):185-196
The first CO2 exposure experiments on several species of pelagic copepods inhabiting surface and deep layers in the western North Pacific
were conducted. Living organisms were collected from two layers between the surface and 1,500 m between latitudes of 11 and
44°N, and they were exposed aboard ship to various pCO2 up to about 98,000 μatm. Mortality of copepods from both shallow and deep layers in subarctic to subtropical regions increased with increasing
pCO2 and exposure time. Deep-living copepods showed higher tolerance to pCO2 than shallow-living copepods. Furthermore, deep-living copepods from subarctic and transitional regions had higher tolerances
than the subtropical copepods. The higher tolerances of the deep-living copepods from subarctic and transitional regions may
be due to the adaptation to the natural pCO2 conditions in the subarctic ocean. 相似文献
87.
The concentration of selenium in marine ferromanganese concretions varies between 0.02 and 1.2 mg kg−1, with an average of 0.6 mg kg−1. This is about two orders of magnitude lower than previously reported. In contrast to minor cationic elements, the concentrations of selenium are relatively uniform between ferromanganese concretions of different origins, except for hydrothermal crusts. It shows the same trends of element enrichment as other oxyanionic elements. The incorporation of selenium into ferromanganese concretions is attributed to adsorption of selenate on iron and manganese oxides. 相似文献
88.
Seasonal and areal variation of continental aerosol in the surface air over the western North Pacific region 总被引:1,自引:0,他引:1
Shizuo Tsunogai Toshitaka Suzuki Takayoshi Kurata Mitsuo Uematsu 《Journal of Oceanography》1985,41(6):427-434
Weekly aerosol samples were collected for two years from 1981 at six stations in the western North Pacific region. The samples were analyzed for aluminum to determine the mineral dust concentration in the air. By combining our data with observations in the central and eastern North Pacific by a US research group, the following results and conclusions have been obtained. Spring peaks in atmospheric mineral dust were observed at all the stations accompanied byKosa episodes (hazes due to mineral dust of Chinese origin). The spring peaks, however, varied from year to year. The mean concentration of mineral dust depends not only on the distance from the Asian coast but also on the latitude of the sampling station. The half-decrease distance of the atmospheric mineral dust turned out to be 500–600 km for all latitudes in the western North Pacific. This indicates that the rate of deposition of mineral dust in the western North Pacific is much larger than that in the central and eastern North Pacific. 相似文献
89.
Ba and Ti in a sediment core (10 m long) from the Okhotsk Sea, covering the last 120 kyrs, were measured. The authigenic Ba
(Baex) contents were calculated and compared with the opal. The correlation coefficient between Baex and opal was quite small (r = 0.34), but it greatly grew larger (r = 0.90), if the Baex contents were multiplied by a simple function increasing with depth, except for two intervals. This may be due to the gradual
change in the sedimentation environment during the glacial ages. One of the exceptional interval is found at 60–170 cm in
depth, corresponding to 10–17 calendar kyr ago, the last termination period of glacial ages, where the Baex began to increase prior to opal. Since the calcium carbonate contents similarly increased prior to the opal increase, the
Baex may be also related to calcareous organisms besides siliceous ones. The other is the last interglacial period around 120
kyr ago when the opal contents were high, but those of the Baex were not increased. This can be explained, if the Baex was reduced to sulfide and dissolved away in a strongly anoxic environment during the biologically productive period. During
the glacial ages, the mass accumulation rate (MAR) of lithogenic Ti was about twice the amount of that during the interglacial
ages. For opal, however, the contrast between the glacial and interglacial ages was more remarkable in its MAR than in its
concentration in sediments, due to the larger variation in the bulk sedimentation rates.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
90.
Shizuo Tsunogai 《Journal of Oceanography》2002,58(2):245-257
The oceanic biogeochemical fluxes in the North Pacific, especially its northwestern part, are discussed to prove their importance
on a global scale. First, the air-sea exchange processes of chemical substances are considered quantitatively. The topics
discussed are sea salt particles transported to land, sporadic transport of soil dust to the ocean and its role in the marine
ecosystem, the larger gas transfer velocity of CO2 indicating the effect of bubbles, and DMS and greenhouse gases other than CO2. Next, chemical tracers are utilized to reveal the water circulation systems in the region, which are the Pacific Deep Water
including its vertical eddy diffusivity, the North Pacific Intermediate Water and the Japan Sea Deep Water. Thirdly, the particulate
transport process of chemical substances through the water column is clarified by analyzing the distribution of insoluble
radionuclides and the results obtained from sediment trap experiments. Fourthly, the northern North Pacific is characterized
by stating the site decomposing organic matter and Si playing a key role in the marine ecosystem. Both are induced by the
upwelled Pacific Deep Water. Fifthly, the oceanic CO2 system related to global warming is presented by clarifying the distribution of anthropogenic CO2 in the western North Pacific, and roles of the upwelled Pacific Deep Water and the continental shelf zone in the absorption
of atmospheric CO2. Finally, Mn and other chemical substances in sediments are discussed as recorders of the early diagenesis and indicators
of low biological productivity during glacial ages in the northwestern North Pacific. It is concluded that the western North
Pacific is characterized mainly by the Pacific Deep Water bringing nutrients to the northern North Pacific, located at the
exit of the global deep water circulation and, therefore, the region plays a key role in the global biogeochemical fluxes.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献