نتایج جستجو برای: distance from sea level

تعداد نتایج: 6309484  

1998

Position: 39°21.9370′N, 72°41.6750′W Start hole: 1400 hr, 29 June 1997 End hole: 1500 hr, 2 July 1997 Time on hole: 73 hr (3.04 days) Seafloor (drill pipe measurement from rig floor, mbrf): 109.5 Total depth (drill pipe measurement from rig floor, mbrf): 416.3 Distance between rig floor and sea level (m): 11 Water depth (drill pipe measurement from sea level, m): 98.1 Penetration (mbsf): 306.8 ...

Journal: :Advances in Space Research 2021

More than 27 years of high precision satellite altimetry enables analysis recent changes in global mean sea level (GMSL). Several previous studies present estimates the trend and acceleration GMSL; however, all are exclusively performed with data from TOPEX/Poseidon, Jason-1, Jason-2 Jason-3 missions (TPJ data). In this study we extend record both time space by including independent ERS-1, ERS-...

Journal: :فیزیک زمین و فضا 0
محمدرضا صلواتی زاده علیرضا آزموده اردلان

sea surface topography (sst) by definition is the separation between the geoid and the mean sea level (msl). the separation between the geoid and msl is caused by various non-gravitational physical effects. if determination of the geoid as the zero point of the height systems from the tide gauge observation be the goal, it is necessary that the affect of the physical effect be precisely compute...

Journal: :environmental resources research 0
mehdi nezhad naderi department of civil engineering, tonekabon branch, islamic azad university ehsanallah hadipour department of civil engineering, tonekabon branch, islamic azad university, tonekabon, iran.

dry areas near the sea can obtain fresh water through solar distillation of saline sea water resources. however, these solar distillation sites produce wastewater as a result of desalination of sea water with high salt concentration. waste must be disposed of with the least effect on the receiving environment (sea, in most cases). initial dilution and its characteristics play important roles in...

2013
Barbara Koeck Josep Alós Anthony Caro Reda Neveu Romain Crec'hriou Gilles Saragoni Philippe Lenfant

Artificial reefs are used by many fisheries managers as a tool to mitigate the impact of fisheries on coastal fish communities by providing new habitat for many exploited fish species. However, the comparison between the behavior of wild fish inhabiting either natural or artificial habitats has received less attention. Thus the spatio-temporal patterns of fish that establish their home range in...

Journal: :Genetics 1983
S A McCommas

The charge-state model of electrophoretic variation was tested by comparing the distances between nearest electromorphs of five enzyme loci within polymorphic species and among pooled species of sea anemone. If the charge-state model is generally true, and in particular if it allows linear distance between electromorphs to be used as a measure of genetic distance, then electromorphs of differen...

Journal: :IOP Conference Series: Earth and Environmental Science 2009

Journal: :journal of rangeland science 2010
m. b. patel r. a. s. patel

main perennial rivers of gujarat, tapi, narmada, mahi and sabarmatiare meeting arabian sea in gulf of khambhat. the out flow of mahi river intothe sea is decreased due to construction of dams like bajaj sagar, kadana, panamand wanakbori weir. so, tidal effect of sea and sea water intrusion is beingincreased on landward side. moreover, due to erratic nature of rainfall andimproper management of ...

Journal: :international journal of environmental research 0
s.m.t. sadatipour islamic azad university, north tehran branch, department of hydrography, tehran, iran r. kiamehr university of zanjan,division of cartography, zanjan, iran m. abrehdary royal institute of technology, division of geodesy and geomatics, stockholm, sweden a.r. sharifi islamic azad university, north tehran branch, department of hydrography, tehran, iran

one of the difficulties in using absolute altitudes is the separation between the mean open sealevel and geoid. theoretically, geoid is the base level in absolute altitudes, but practically, the mean open sealevel is used as a base level for absolute altitudes. the difference between these two levels is called as the seasurface topography. in this research, it is dealt the mean sea level modeli...

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