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日本人が判断しにくい類語の使い分けを、約15万件の英語科学論文データ(全て米英国より発表分)に基づき分析。ネイティブの使う単語・表現が詰まっています。論文から引用した生の例文も満載で、必ず役立つ1冊。
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いられている類似度計算アルゴリズムについて触れ, しては,(“store + V" (PP“in”(* - N")というパターン. 問題提起を行う。 (図1のC1)に. 解釈1:(“store-V" (PPin") frepository +N) SENA では,単語の直接の同義語と上位語を類似度計. 解釈2:(“program +N”.


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敷金・礼金って英語でなんて言うの? - DMM英会話なんてuKnow? Depositという単語の同義語


アパートやフラットの賃借の手順がどんなものなのかよく知らない人は、今からご紹介する8つの基本的な英単語や熟語を読んでみてください。 1.. 1/2 bedroomsなどの表現が書かれた物件を見かけたら、それは一つの部屋は実際には居間だという意味です。. Damage deposit. Next【英語の語彙力アップ】yesの同義語・類語を考えてみよう ».
プレミアム高解像度ストックフォト、ベクター画像、イラストや動画の数百万のDepositphotosコレクションから、ロイヤリティーフリーの愛という言葉の同.
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glossary



negotiable certificate of depositの同義語. NCD; CD; certificate of deposit. negotiable certificate of depositに関する情報. 「譲渡性有価証券(negotiable security)」は、marketable securityとも呼ばれ、アメリカでは簡単に投資家の間で転売できるという.
というテキストは、「A社の社長がアメリカに行った」という. NEC技報 Vol.65 No.2/2012. 同義語抽出技術では、同じ意味の単語を抽出することで、. 表現のバリエーションを. deposit”→“FCD”から「外貨預金」と「FCD」)するなど、. 多段階変換も行います。

Also used to express the quantity lost by these processes.
Analogue models in hydrology most frequently simulate the flow of water in a channel or through a porous medium by the flow of electric current through a circuit composed of resistors and capacitors.
The weight given each day's precipitation is usually assumed to be an exponential or reciprocal function of time, with the most recent precipitation receiving the greatest weight.
Antidunes commonly move upstream.
It is often denoted by a bar, e.
The direction is measured downslope normal to the contours of elevation relative to geographic north.
It is assumed to be equal in amount to the residual water after drainage.
It is normally taken as the water in the soil between wilting point and field capacity.
In this context water holding capacity of a soil is used and is identical to the available water.
Generally, it purports to represent or to summarize the relevant features of a set of values, e.
In a more limited sense, an average compounds all the values of the set, e.
The shore inland from the water line to the place where there is a marked change https://jackpot-bonus-list.site/4/4149.html material or physiographic form, or to the line of permanent vegetation.
Bed material particles may be moved momentarily or during certain flow conditions.
The instrument may be operated from the bank or from a cabel carrying personnel.
Sometimes defined as relative decrease in height.
Darcy coefficient see also hydraulic conductivity; permeability coefficient Numerical value expressing the hydraulic conductivity.
It is used as an indicator of the presence of organisms potentially capable of causing disease in man.
The proportions are usually based on time or flow measurements.
Hydrological conceptual models are used for simulation of the behaviour of a basin.
Also includes all activities where the use of water results in loss of the original water supplied, such as industrial or community consumption.
The product-moment correlation coefficient is the covariance of the variates divided by the product of their standard deviations.
Traditionally the term refers to instruments with cups or propellers.
Darcy's formula see also hydraulic conductivity Law expressing the proportionality of the specific discharge of a liquid flowing through a porous medium to the hydraulic gradient under laminar flow low Reynold number conditions.
It may occur in the place where it is produced, or it may be transported by streams or ice and deposited in other localities.
It consists of material lying on steeper slopes than an allvial fan.
For a given period months, years algebraic sum of the degree-days of the different days of the period.
Often implies the removal of the soil down to the bedrock.
Removal, by natural or artificial means, of all vegetation and organic matter.
Detention storage includes surface and channel detention but does not include depression storage.
It includes surface flow and interflow and is used where interflow cannot be separated in hydrological analyses.
When a given direction coincides with that of the specific discharge, the directional hydraulic conductivity in that direction is the ratio of the specific discharge to the projection of the hydraulic gradient in that direction; when the given direction coincides with that of the hydraulic gradient, it is the ratio of the projection of the specific discharge in that direction to the hydraulic gradient.
Its volume is equal to rainfall excess.
Some procedures for its derivation include prompt subsurface runoff but all exclude base flow.
An index of hydrological drought corresponding to levels below the mean in streams, lakes reservoirs, and the like.
However, an index of agricultural drought must relate to the cumulative effects of either an absolute or an abnormal transpiration deficit.
Dunes move downstream at velocities that are small compared to the streamflow velocity.
It is a ノルウェーのカジノ of the saturation.
It is expressed as the ratio of the volume of the interconnecting interstices to the gross volume of the porous medium, inclusive of voids.
In some procedures the prompt subsurface runoff is entirely excluded from direct runoff and then effective rainfall is equal to rainfall excess.
There is no imputation of mistake.
Commonly used extreme ラジオ版のゴールドディガーゲーム distributions are Frechet, Gumbel and Weibull.
TR 3 Difference of water levels at the two sides of a weir or other hydraulic control structure.
The length of the fetch area is measured in the direction of the wind.
The drop of potential between adjacent equipotential lines is constant and the spacing between neighbouring streamlines is such that the flow rate is the same between each pair.
It may be used to store water in relatively small quantities to take care of variations in the demand for water which occur over short periods of time, usually not exceeding several hours.
In rivers and lakes it is formed in supercooled turbulent waters.
It is free to move by capillary action or under the force of gravity.
Ghyben-Herzberg lens Freshwater body floating depositという単語の同義語 saline groundwater.
Usually expressed in units of height.
In open channels, flow is subcritical, critical or supercritical if its Froude number is less than, equal to or greater than unity respectively.
It is used interchangeably with the terms stage and water level.
It is based on the exponential behaviour of frequency distribution curves for low frequencies log-log law of representation and assumes storms large enough to saturate the soil.
Well graded implies a more or less uniform distribution from coarse to fine: poorly graded implies uniformity in size or lack of a continuous distribution.
Sometimes depositという単語の同義語 around drainage pipes.
Hele-Shaw model; parallel-plate model Analogue based on the similarity between two-dimensional plane groundwater flow and the flow of a liquid between two parallel plates of which at least one is transparent チュニカで最高のカジノペイアウト a capillary interspace.
There is no imputation of mistake.
Commonly used extreme value レーザー金属蒸着 are Frechet, Gumbel and Weibull.
TR 3 Difference of water levels at the depositという単語の同義語 sides of a weir or other hydraulic control structure.
The length of the fetch area is measured in the direction of the wind.
The drop of potential between adjacent equipotential lines is constant and the spacing between neighbouring streamlines is such that the flow rate is the same between each pair.
It may be used to store water in relatively small quantities to take care of variations in the demand for water which occur over short periods of time, usually not exceeding several hours.
In rivers and lakes it is formed in supercooled turbulent waters.
It is free to move by capillary action or under the force of gravity.
Ghyben-Herzberg lens Freshwater body floating above saline groundwater.
Usually expressed in units of height.
In open channels, flow is subcritical, critical or supercritical if its Froude number is less than, どのようにスロットマシンで勝つのですか depositという単語の同義語 or greater than unity respectively.
It is used interchangeably with the terms stage and water level.
It is based on the exponential behaviour of frequency distribution curves for low frequencies log-log law of representation and assumes storms large enough to saturate the soil.
Well graded implies a more or less uniform distribution from coarse to fine: poorly graded implies uniformity in size or lack of a continuous distribution.
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Hele-Shaw model; parallel-plate model Analogue based on the similarity between two-dimensional plane groundwater flow and the flow of a liquid between two parallel plates of which at least one is transparent with a capillary interspace.
In particular, charting the open bodies of water for navigational purposes.
An inverse reaction to salt formation.
It is remote from surface influences and has a relatively small temperature gradient.
Examples are run-of-the river hydroelectric power generation, navigation, water quality improvement, fish breeding, and recreation.
It is separated from the saturated zone by an impermeable bed.
Often a family of curves is shown, each depicting a specific occurrence frequency or return period in years.
It moves through the upper strata of a formation at a rate much in excess of normal base-flow seepage.
IGH 0710 isonival syn.
In channel flow the fluid particles move approximately in definite, relatively this web page paths with no significant transverse mixing.
The Reynolds number is smaller than 500-2000 in flow in channels and smaller than 1-10 in flow through porous media.
In groundwater flow describing the flow of an incompressible, homogeneous fluid through a homogeneous, isotropic non-deformable porous medium, the variable in the equation is the piezometric head or potential.
TR 0737 leaching see also leaching requirement 1 Removal of salts from upper soil layers by relatively salt-free water.
Leaching requirement is used primarily under steady state or long-time average conditions.
GHP 2 Flow into depositという単語の同義語 reservoir of the local streams draining into it.
Galton distribution Transformed normal probability distribution in which the variate is replaced by its logarithm.
The upper surface of such a stream stands higher than the water table or other potentiometric surface of the カジノハイローラースロット to which it contributes.
DST 0766 marsh syn.
DST 0776 mean monthly discharge see also multi-annual mean Arithmetic mean of all the individual monthly mean discharges for a named month in a period of record.
The total discharge is the product of that distance by the sum of the products of the mean read article the depths of two adjacent verticals by the mean of the average velocities over those two verticals.
For n discrete data, the middle value of the ranked data if n is odd, or the mean of the two central values if n is even.
DST 0781 medium-term extended hydrological forecast Forecast of the future value of an element of the regime of a water body for a period ending between two and ten days from the issue of the forecast.
The total discharge source the sum of the products of the average velocity in each vertical by the depth of that vertical and by the mean width of the two panels adjacent to the vertical.
In a distribution of a continuous variate, the variate with maximum probability density.
In hydrology, a model is in most cases mathematical representation of a basin, a water system, a series of data, etc.
For a distribution of a variate, moments may be taken about the origin or about a given fixed value; if the latter is the mean, the ミラーボールスロット are central moments.
DST 0805 monitoring syn.
Multi-annual mean monthly discharge for April is the arithmetic mean of all April monthly mean discharges for a number of years.
DST 0821 multispectral remote sensing Remote sensing in two or more spectral bands, such as visible and infrared.
The surface is commonly hummocky.
In Alaska: more widely applied to any mossy and swampy ground regardless of topographic environment.
Gaussian distribution Mathematically defined, symmetrical, bell-shaped continuous probability distribution traditionally assumed to represent random errors.
TR 0846 normal hydrological value 有名なバービーゲーム無料オンライン value of a hydrological グランドカジノオクラホマ州の仕事 taken over a period アンドロイド携帯電話用無料ゲーム by consensus such that the mean over any longer period does not significantly differ from the value obtained.
DST 0870 overdraft Amount of water withdrawn from a water resources system in excess of the optimal yield.
For example fitting a rainfall-runoff model to a particular catchment will involve https://jackpot-bonus-list.site/4/4114.html parameter values appropriate to that catchment.
There is a positive correlation between successive values when arranged in the order of their occurrence.
Used as an indicator of acidity pH 7.
The speed of the liquid can be determined from the difference between the dynamic pressure and the static pressure.
Smallest element on the ground distinguishable on an image acquired by remote sensing.
Occurs mainly in karst areas.
It includes fluvial dynamics and all the phenomena related to erosion of and sedimentation on the stream bed.
It thus includes evaporation from the soil and transpiration from the vegetation of a specified region in a given time interval, expressed as depth.
TR 0938 pressure head Height of a column of static water that can be supported by the static pressure at a point.
Such a station is usually equippe with recording instruments.
TR 0943 probabilistic process see also stochastic process Process in which the probability of occurrence of the variables is taken into account, whereas their sequence of occurrence is ignored.
DST 0945 probability distribution see also frequency distribution Distribution giving the probability of a value of a variate as a function of the variate.
DST 0946 probability of forecast The chance of occurrence of a quantified assessment in real time of future events.
One half of a normal sampling distribution lies within 0.
GHP 0950 propeller-type current meter Current meter the rotor of which is a propeller rotating around an axis parallel to the flow.
It consists of two thermometers, one of which the dry bulb is an ordinary glass thermometer, while the other wet bulb has its bulb covered with a jacket of clean muslin which is saturated with distilled water prior to an observation.
The initial stage consists of patches of melted snow.
The data are used for determining the aquifer parameters in the vicinity of the pumped well.
DST 0959 quantitative precipitation forecast QPF Forecast of precipitation amount.
DST 0978 random process see also stochastic process Generally synonymous with the more usual and preferable "stochastic process".
Sometimes employed to denote a process in which the movement from one state to the next is determined by a variable which is independent of the initial and final state a pure random process.
If digitized, it is a rating table.
Ideally the records should be of sufficient length to enable the identification of secular changes of climate.
The most common form of regression analysis is linear regression.
For a first degree linear regression.
GHP 2 Basin where intensive hydrological studies are conducted under relatively unchanged conditions.
For example, in a linear regression, the difference between an observed value and the value determined from the equation.
It may be expressed in line pairs per millimetre or click, or in many other manners.
GHP 1028 Reynolds number Dimensionless number expressing the ratio of inertia forces to viscous forces.
Discontinuous motion of sediment particles above the ground in flow of air or above the channel bed in flow of water.
It can occur either in surface or groundwater bodies.
DST 1061 sandbox model Physical model simulating a porous medium in which the flow domain in the prototype porous medium is represented by a flow domain in a porous medium with reduced physical dimensions.
Derivation of the statistical distribution of a time series is a typical example of secondary data processing.
In watercourses, sediment is the alluvial material carried in suspension or as bed load.
It includes bed load as well as suspended 最高の無料ブラックジャックソフトウェア />Usually expressed in weight per unit of time.
It is the average actual velocity of an unsaturated flow.
In hydrology this concept is used with respect to measuring devices, catchment models, etc.
DST l092 serial correlation coefficient Sample value of the parent autocorrelation coefficient.
It may be a combination of the liquid or water-carried domestic, municipal and industrial wastes, together with such groundwater, surface water and storm water as may be present.
Included with sheet erosion, however, are the numerous but conspicuous small rills that are caused by minor concentrations of runoff.
The region immediately landward of the shore-line is the coast, 王の戦いゲームオンライン無料 seaward from this line is the shore.
Showers are characterized by their sudden beginning and ending, and generally by large and rapid changes of intensity.
It generally implies water loss in a closed depression or blind valley.
This results in a pressure less than atmospheric in that portion and hence requires that a partial vacuum be created to start flow.
A siphon utilizes atmospheric pressure to effect or increase the flow of water it carries.
It may occur naturally in karstic regions.
The most commonly used is the Manning equation.
The freshly fallen snow can then be readily identified and extracted and its depth measured.
The mass includes liquid water content and the volume includes natural air spaces.
MRS 1179 spill syn.
GHP 2 Maximum flood flow that could be passed without damage or serious threat to the stability of engineering structures.
TR 1191 squall see also squall line Atmospheric phenomenon characterized by a very large variation of wind speed, beginning suddenly, which has a duration of the order of minutes, and decreases rather suddenly in speed.
Often accompanied by a shower or thunderstorm.
DST 1200 standard error see also probable error; standard deviation; standard error of estimate Positive square root of the variance of the sampling distribution of a statistic.
DST 1201 standard error of estimate s.
DST 1202 standardized variate Value of a variate reduced to standardized form zero mean unit variance by subtracting the population or sample mean and then dividing by the population or sample standard deviation.
From the Earth, the satellite thus appears to be stationary over a point on the Earth.
It is said to be stationary in the wide sense or to the second order if the mean check this out variance are independent of time.
The statistics of samples drawn from a stationary process may vary due to sampling variability but not due to their size or their position in the population.
In most cases, s and t refer to time but they may also refer to space.
It includes interception by vegetal cover, depression storage, and evaporation during precipitation, but does not include surface detention.
If in a channel it passes along the channel as a wave.
It may be undulating or breaking.
DST 1263 tailrace Channel which conducts water away from a water-wheel or turbine.
It may have any shape, e.
It is expressed as the product of the hydraulic conductivity and the thickness of the saturated portion of an aquifer.
Unit used to express tritium concentrations.
One tritium unit is a concentration of one tritium atom in 10 18 hydrogen atoms.
It is an ideal value which could be known only if all causes of error were eliminated.
TR 1310 tsunami see also earthquake flood Great sea wave produced by a submarine earthquake or volcanic eruption.
In channel flow, it occurs at Reynolds number larger than approximately 5000, thanks ラスベガスのヤシの木カジノ opinion in flow through porous media at Reynolds number larger than 10.
DST 1332 variance see also moment; standard deviatiion Second central moment of a frequency distribution.
For a set of values the sum of the squares of the deviations from the mean divided by the number of values.
DST 1334 varied flow see also non-uniform flow Flow occurring in streams having a variable cross section or slope.
It is usually expressed as a coefficient.
Note: This may be used from boats or ice cover at shallow depth.
TR 1350 wash load Relatively fine material, in near-permanent suspension in a stream system, which is transported entirely through the system without deposition.
In nature it contains small amounts of heavy water, gases and solids mainly salts in solution.
GHP 1371 water management Planned development, distribution and use of water resources.
DST For example, the areal rainfall computed by the Thiessen polygon method.
Excess drawdown may be influenced by the factors of design and construction of the production well.


Should we simplify spelling? (with English subtitles)


476 477 478 479 480

日本人が判断しにくい類語の使い分けを、約15万件の英語科学論文データ(全て米英国より発表分)に基づき分析。ネイティブの使う単語・表現が詰まっています。論文から引用した生の例文も満載で、必ず役立つ1冊。


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