• 한국연초학회지
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• 제7권1호
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• pp.15-23
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• 1985

Growth response and evapotranspiration of tobacco as to each soil moisture condition treated with different height of ground water table such as 30cm, 100cm, 170cm, and 230cm were investigated. The results obtained were as follows; 1. Soil water potential in the rhizosphere (25cm depth from surface) treated with ground water table (G.W.T) of 230 cm was less than -6.5 bar at 60 days after transplanting. 2. Dry weight of leaves per plant was the highest in the pot treated with 100 cm G.W.T and was the lowest in the pot treated with 230 cm G.W.T.. Leaves/Stem ratio of dry weight was the lowest in the pot treated with 230 cm G.W.T. This would show that extension of leaves as compared with elongation of stem was suppressed. .3. In the roster stress condition of 230 cm G.W.T., extension of leaves was continued until the latter growth stage, Relative growth rate of leaf area per plant of the pot with 30 cm G.W.T. was the highest through all growth period after fixation of G.W.7., but owing to lower density of leaf, the dry weight of leaves per plant was less rather than that of the pot with 170 cm G.W.T. at 64 days after transplanting. 4. The highest evapotranspiration per plant per day was shown at the 45th day after transplanting in the pots with 30cm and 100cm G.W.T. and at 60 days in the pots with 170cm and 230cm G.W.T respectively. 5. In the soil moisture conditions with 30cm and 100cm G.W.T., evapotranspiration per plant per hour was much higher in the daytime that at night as well as in clear day than in rain-cloudy day owing to loner relative humidity , but in the water stress condition with 230 cm G.W.T., that was much lower. 6. Total evapotranspiration per plant during the whole growing period of 64 days was in order of 30cm > 100 cm > 170 cm > 230 cm G.W.T.. Total evapotranspiration for 34 days after fixation of G.W.T was much higher at night than in the daytime in case of water stress conditions i.e 170cm and 230cm G.W.T. but in normal condition of the pots with 30cm and 100cm G.W.T. that was much higher in the daytime than at night. 7. Leaf water potential of the 3rd and 6th leaf from top at 64 days after transplanting was in order of 100cm > 30 cm > 170cm > 230cm G.W.T. The reason why leaf water potential in the pot with 30cm was less than that in the pot with 100cm G.W.T. would be the abnormal turgidity with low density of cell substrates by the excess water absorption in the pot with 30cm G.W.T..

• 대한토목학회논문집
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• 제37권2호
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• pp.303-310
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• 2017

증발산량은 수자원 부존량 평가, 물수지 분석, 지구의 물 순환 및 에너지 순환을 이해하기 위해서 알아야 할 중요한 수문량이다. 실제 증발산량이 습윤조건의 증발산량의 2배에서 잠재 증발산량을 제한 것과 같다는 보완관계(Complimentary relationship)를 기반으로 기상관측망 지점에서 일반적으로 관측되는 기상 자료를 이용해 증발산량을 산정하는 방법이 다양하게 개발되어 왔다. 이 중 Granger and Gary (GG)방법은 보완관계를 기반으로 경험적인 매개변수를 도입하여, 지역의 기온 등의 자료만 활용하여 증발산량을 산정할 수 있도록 하는 경험식이다. 본 연구에서는 FLUXNET2015 자료 중 아시아 지역 내의 10개 지점에서 에디공분산법을 활용해서 관측된 증발산량 자료를 GG방법을 활용하여 산정한 증발산량과 비교하였다. 내륙지역의 경우 해안지역에 비해 상대적으로 정확하게 증발산량이 추정되었고, 이에 해안지역의 경우에만 담금질 기법(Simulated Annealing, SA)을 활용하여 GG방법의 매개변수를 수정하였다. 수정된 GG방법을 활용하여 증발산량 추정 결과의 Root mean square error, Coefficient of determination($R^2$), Mean absolute BIAS를 개선할 수 있었다.

• 한국농공학회논문집
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• 제53권4호
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• pp.39-47
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• 2011

The aim of the study is to predict potential evapotranspiration and crop water requirement using meteorological data from MIROC3.2 with A1B scenario. Increase of evapotranspiration due to temperature rise can be observed out of the analysis, while effective rainfall decreased. The evapotranspiration elevation results in large amount of crop water requirement in the paddy farming. It can be seen that rainfall intensification at non-irrigation period brings effective rainfall decrease, while contributes to higher demand of crop water at irrigation period. It is necessary to secure additional water resources to adapt the climate change. It is expected that estimation on potentialevapotranspiration in this study can be used for formulation of master plan of water resources.

• 한국농공학회논문집
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• 제60권3호
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• pp.15-25
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• 2018

Estimating the reference evapotranspiration is an important factor to consider in irrigation system design and agricultural water use. However, there is a limitation in using the FAO Penman-Monteith (FAO P-M) equation, which requires various meteorological data. The purpose of this study is to compare three reference evapotranspiration (ETo) equations in the case of meteorological data missing for 11 study weather stations. Firstly, the FAO P-M equation is used for reference potential evapotranspiration estimation with the actual solar radiation data $R_n$ and the actual vapor pressure $e_a$. Then, in the case of $R_n$, and $e_a$ are missed, the reference evapotranspirations applying FAO P-M, Priestley-Taylor (P-T), Hargreaves (HG) equation were calculated using other meteorological factors. Secondly, MAE, RMSE, $R^2$ were calculated to compare ETo relationship from the ETo equations. From the results, ETo with Hargreaves equation in coastal areas and the Priestley-Taylor equation in the inland areas showed relatively high correlation with FAO P-M when $e_a$ data is missed. In the case of $R_n$ data is missed or two weather data, $e_a$, and $R_n$ data are all missed, $R^2$ value in Priestley-Taylor equation was highest in coastal areas, and $R^2$ values in Hargreaves equation were the high values for 7 inland areas. The results of sensitivity analysis showed that net radiation was the most sensitive for P-T and HG equation, and for FAO P-M, the most sensitive factor was net radiation and relative humidity, air temperature and wind speed were follows. Therefore, in considering of the accessibility to the coast, the types of the missing wether data, and the correlation and the magnitude of error, the reference evapotranspiration equations would be selected in sense of different conditions.

• 대한공간정보학회지
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• 제14권2호
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• pp.55-62
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• 2006

현재 물부족 국가로 분류되고 있는 우리나라 현실에서 가뭄은 재해 관리에 있어서 중요한 요소가 되고 있다. 위성영상은 광역의 지표면에 대해 오랜 시간 동안 주기적으로 자료를 취득할 수 있게 해주므로, 이를 가뭄의 관측에 활용하면 유용한 결과를 얻을 가능성이 크다. 본 연구에서는 광역의 가뭄현상을 해석하는 데 있어서 위성영상을 활용하는 방안을 제시하고자 하였다. 따라서, 미국 NASA에서 제공하는 MODIS 자료의 식생지수(NDVI)자료를 이용하여 광역의 증발산량을 산정하는 방법을 개발하였다. 위성영상을 이용하여 산정된 증발산량 분포를 강우 분포자료 및 잠재증발산량 분포자료와 결합하여 기후학적 물수지를 산정하였으며, 이를 기반으로 대상지역의 가뭄을 효과적으로 분석할 수 있었다. 본 연구의 결과는 가뭄 해석에 있어서의 위성영상의 활용도를 높이는 데 기여를 할 것이다.

• Water Engineering Research
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• 제5권1호
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• pp.1-16
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• 2004

The purpose of this study is to understand the characteristics of hourly PET(Potential Evapo Transpiration) variation estimated using Penman ET model. The estimated PET using Penman model was compared with measured ET. For this study, two subwatersheds were selected, and fluxes, meteorological data and soil moisture data were measured during the summer and winter days. During the winter days, the aerodynamic term of Penman ET is much greater than that of energy term of Penman ET for dry soil condition. The opposite phenomena appeared fer wet soil condition. During the summer days, energy term is much more important factor for ET estimation compared with aerodynamic term regardless of soil moisture condition. Penman ET, measured ET, and energy term show the similar hourly variation pattern mainly because the influence of net radiation on the estimation of Penman ET is much more significant compared with other variables. Even though there are much more soil moisture in the soil during the wet days, the estimated hourly ET from Penman model and measured hourly ET have smaller values compared with those of dry days, indicating the effect of cloudy weather condition.

• Water Engineering Research
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• 제5권3호
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• pp.123-131
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• 2004

This paper describes the use of spatial interpolation for estimating seasonal crop potential evapotranspiration (PET) and irrigation water requirement in unmeasured evaporation gage stations within Edwards Aquifer, Texas using GIS. The Edwards Aquifer area has insufficient data with short observed records and rare gage stations, then, the investigation of data for determining of irrigation water requirement is difficult. This research shows that spatial interpolation techniques can be used for creating more accurate PET data in unmeasured region, because PET data are important parameter to estimate irrigation water requirement. Recently, many researchers are investigating intensively these techniques based upon mathematical and statistical theories. Especially, three techniques have well been used: Inverse Distance Weighting (IDW), spline, and kriging (simple, ordinary and universal). In conclusion, the result of this study (Table 1) shows the kriging interpolation technique is found to be the best method for prediction of unmeasured PET in Edwards aquifer, Texas.

• 한국수자원학회논문집
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• 제48권11호
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• pp.915-923
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• 2015

본 연구에서는 유역 물수지 방법을 기반으로 제주도 지역에 적합한 용수량 산정방법을 제안하고, 이를 기반으로 4개 하천유역에 대해 지역 및 고도에 따른 증발산량, 용수량 특성을 평가하였다. SWAT-K 유역모형을 적용하여 1992~2013년 기간에 대해 잠재증발산량과 실제증발산량을 산정하고, 이로부터 유역의 순물소모량을 추정하였다. 고도증가에 따라 잠재증발산량은 선형으로 감소하는 반면, 실제증발산량은 강수량에 의한 토양내 가용수분의 증가로 인해 약 400m 고도까지는 증가하다가 이후 고도에서는 식생, 가용수분의 감소, 저온현상 등으로 인해 감소하는 것으로 나타났다. 고도에 따른 순물소모량은 강정천유역을 제외한 3개 유역에서 고도증가에 따라 순물소모량이 선형적으로 감소하는 것으로 나타났으며, 고도 200m 이하 작물경작지에서의 순물소모량은 연간 559~680m로 분석되었다. 추정된 용수량을 실제 관정 이용량과 비교한 결과, 여름철(6~8월) 양수량은 급수관행으로 인해 크게 증가하는데 비해, 작물경작에 따른 순물소모량은 오히려 감소하는 것으로 나타났다. 이에 대해서는 향후 더 많은 관정 이용량과 추가적인 대상지역을 반영하여 분석이 필요할 것으로 판단된다.

• 한국토양비료학회지
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• 제44권5호
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• pp.674-678
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• 2011

1. 최근 30년간 우리나라 67개 지역 전체의 평균 PET는 $2.36mm\;day^{-1}$이었다. 2. 우리나라 67개 지역의 년중 일평균 PET 범위를 분석한 결과 $1.42{\sim}3.45mm\;day^{-1}$이었으며, 그중 23개의 지역이 $2.01{\sim}2.20mm\;day^{-1}$의 범위에 속하였다. 3. 본 연구대상 7개 지역의 잠재증발산량 차이를 분석한 결과, 30년간 평균 PET는 서울이 $1.97mm\;day^{-1}$이었고, 여수는 $2.60mm\;day^{-1}$로 높았으며, 7개 지역 평균은 $2.24mm\;day^{-1}$이었다. 4. 우리나라 지역별 잠재증발산량 변동 양상을 예측할 수 있는 $y=a+b{\cdot}sin[(2{\pi}/c)x+d]$ 모형을 개발하였다. 5. 지역별 잠재증발산량 변화주기는 16년~32년으로 지역별 변이가 크며, 여수가 32.1년으로 주기가 길며, 부산은 변화주기의 유의성이 없었다.

• 농업과학연구
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• 제46권1호
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• pp.137-149
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• 2019

Accurate estimation of reference evapotranspiration (RET) is important to quantify crop evapotranspiration for sustainable water resource management in hydrological, agricultural, and environmental fields. It is estimated by different methods from direct measurements with lysimeters, or by many empirical equations suggested by numerous modeling using local climatic variables. The potential to use some such equations depends on the availability of the necessary meteorological parameters for calculating the RET in specific climatic conditions. The objective of this study was to determine the proper RET equations using limited climatic data and to analyze the temporal and spatial trends of the RET in South Korea. We evaluated the FAO-56 Penman-Monteith equation (FAO-56 PM) by comparing several simple RET equations and observed small fan evaporation. In this study, the modified Penman equation, Hargreaves equation, and FAO Penman-Monteith equation with missing solar radiation (PM-Rs) data were tested to estimate the RET. Nine weather stations were considered with limited climatic data across South Korea from 1973 - 2017, and the RET equations were calculated for each weather station as well as the analysis of the mean error (ME), mean absolute error (MAE), and root mean square error (RMSE). The FAO-56 PM recommended by the Food Agriculture Organization (FAO) showed good performance even though missing solar radiation, relative humidity, and wind speed data and could still be adapted to the limited data conditions. As a result, the RET was increased, and the evapotranspiration rate was increased more in coastal areas than inland.