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194 results for “Tributaries”
Distribution. Brazilian Amazon, S from the Rio Iriri at least as far as the S (left) margin of the Rio Peixoto de Azevedo (E tributary of the Rio Teles Pires), the S limits are not beyond the headwaters and upper Rio Paraguay (c.14° 30' S), the upper Rio Teles Pires evidently marks the W limit. in Callitrichiade
Distribution. Brazilian Amazon, S from the Rio Iriri at least as far as the S (left) margin of the Rio Peixoto de Azevedo (E tributary of the Rio Teles Pires), the S limits are not beyond the headwaters and upper Rio Paraguay (c.14° 30' S), the upper Rio Teles Pires evidently marks the W limit.
Distribution. Limited to the Amazon River Basin and most ofits tributaries in Colombia, Ecuador, and Peru. It may also extend into the Orinoco River system in Venezuela, but itis uncertain if sightings there were this species or the Guiana Dolphin (S. guianensus). in Delphinidae
Distribution. Limited to the Amazon River Basin and most ofits tributaries in Colombia, Ecuador, and Peru. It may also extend into the Orinoco River system in Venezuela, but itis uncertain if sightings there were this species or the Guiana Dolphin (S. guianensus).
Distribution. Brazilian Amazon, N of the rios Solimoes and Japura, from the confluence with the Rio Negro in the E, and as far W as the Rio Apaporis, a left (N) bank tributary of the Japura, the N limit is the Negro/Uaupés river system. Its distribution may extend into SE Colombia between the rios Apaporis and Vaupés, where it probably intergrades with the distribution of the White-chested Titi (C. lugens), although there are no data on the ranges of either species from this region. in Phitheciidae
Distribution. Brazilian Amazon, N of the rios Solimoes and Japura, from the confluence with the Rio Negro in the E, and as far W as the Rio Apaporis, a left (N) bank tributary of the Japura, the N limit is the Negro/Uaupés river system. Its distribution may extend into SE Colombia between the rios Apaporis and Vaupés, where it probably intergrades with the distribution of the White-chested Titi (C. lugens), although there are no data on the ranges of either species from this region.
Distribution. Amazonian Brazil, between the lower Rio Jurua and the lower Rio Purus, both S bank tributaries of the upper Rio Solimoes-Amazonas in Amazonas State. in Phitheciidae
Distribution. Amazonian Brazil, between the lower Rio Jurua and the lower Rio Purus, both S bank tributaries of the upper Rio Solimoes-Amazonas in Amazonas State.
F in The Simuliidae (Diptera) of the River Oder and its tributaries, with special reference to the re-appearance of Simulium (Schoenbaueria) nigrum (Meigen) in larger rivers in Central Europe
F. 3. Breakwaters on the lower course of the Oder at Reitwein (52°29.932 N, 14°37.823 E) during high water levels.
FIGURES 14–19. Delicatophycus liuweii, SEM. External views. 14–15 in Delicatophycus liuweii sp. nov., a new cymbelloid diatom (Bacillariophyceae) from an upper tributary of the Liujiang River, Guangxi, China
FIGURES 14–19. Delicatophycus liuweii, SEM. External views. 14–15. External view of a whole valve. 16–17. Show the varied areolae at apices. 18–19. External view of valve center showing striae composed of areolae, 3–6 stigmata, and the proximal raphe endings. Scale bars =2 μm.
FIGURES 1–13 in Delicatophycus liuweii sp. nov., a new cymbelloid diatom (Bacillariophyceae) from an upper tributary of the Liujiang River, Guangxi, China
FIGURES 1–13. Delicatophycus liuweii LM. Valve views showing size diminution series for the species. Fig. 1 is the holotype. Scale bar =10 μm.
FIG. 1 in Ecosystem Functions of a Spring-Fed Tributary in Providing Foraging Habitat and Thermal Refuge for Juvenile Masu Salmon
FIG. 1. Photographs of the spring-fed tributary (A) and runoff tributary (B) reaches in the Shubuto River System, Kuromatsunai Town, Hokkaido, Japan.
FIG. 4 in Ecosystem Functions of a Spring-Fed Tributary in Providing Foraging Habitat and Thermal Refuge for Juvenile Masu Salmon
FIG. 4. Relationship between total biomass of stomach contents and standard body length of juvenile Oncorhynchus masou masou in each sampling event.
Application of Transcriptomics Dose-Response Modeling to Risk-Based Prioritization of Contaminants Detected in Tributaries of the North American Great Lakes
GEO Series GSE268998. Raphidocelis subcapitata. 270 samples. Type: Expression profiling by high throughput sequencing.
Effects-based Monitoring of Contaminants of Emerging Concern in Great Lakes Tributaries: Calculating the Risk of Fish Developing Liver Toxicity and Cancer
GEO Series GSE146903. Homo sapiens. 71 samples. Type: Expression profiling by high throughput sequencing.
Application of Transcriptomics Dose-Response Modeling to Risk-Based Prioritization of Contaminants Detected in Tributaries of the North American Great Lakes [D. magna]
GEO Series GSE269991. Daphnia magna. 335 samples. Type: Expression profiling by high throughput sequencing.
Hydrologic future scenarios for the main Nile tributaries.
<p><span>The water supply model considers four main tributaries to the Nile: Blue Nile, White Nile, Dinder-Rahad and Tekeze-Atbara.</span></p> <p><span>Starting from future time series created according to three RCPs scenarios (RCP2.6, RCP4.5 and RCP8.5), a large ensemble of uncertain streamflow is generated by altering the timing and magnitude of extremes (Quinn, J. D., et al. Exploring how changing monsoonal dynamics and human pressures challenge multireservoir management for flood protection, hydropower production, and agricultural water supply. Water Resources Research, 2018, 54.7: 4638-4662). Future streamflows are derived from IPCC 5<sup>th</sup> assessement’s projections of temperature and precipitation using the HBV model and altered by first fitting the monthly means in a Fourier decomposition and then applying perturbations on amplitudes and phases to strengthen the magnitude of extremes and/or their timing. </span></p> <p><span>For each combination of tributary and RCP, 100 different realizations of the monthly streamflow of a 94-year-long time series are generated.</span></p> <p><span>Data are divided based on tributaries and climatic scenarios. In each file, every row is one of the 100 different realizations of the monthly streamflow time series, while each column contains the monthly streamflow of the river reported in m<sup>3</sup>/s starting from January 2007 in the first column until December 2100</span><span> in the last</span><span>. </span></p> <p><span> </span></p>
The nonstationary research of flood coincidence of Huai River and its tributaries based on copula function.
<p>The daily streamflow data extracted from3 selected stations from the Huaihe Basin, China.</p>
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