2 edition of Area-time structure of the monthly precipitation process found in the catalog.
Area-time structure of the monthly precipitation process
|Statement||by Vujica Yevjevich and Alan K. Karplus.|
|Series||Hydrology papers -- 64|
|Contributions||Karplus, Alan K., Colorado State University.|
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Additional Physical Format: Online version: Yevjevich, Vujica M., Area-time structure of the monthly precipitation process (Online) (OCoLC) The monthly totals of precipitation of 21 Greek stations for the period as well as the calendar of classification of th e types circulation were studied (Maheras, ).
Yevjevich V, Karplus AK () Area-time structure of the monthly precipitation process, Hydrology Paper No. Colorado State University, Fort Collins Google Scholar Yule G () On a method of investigating periodicities in disturbed series, with special application to Wolfert’s sun spot numbers.
Stachastic structure of water use time series by Jose D. Dalas-LaCruz and V. Yevjevich 0 Area time structure of the monthly precipitation process by ich and Alan K.
Karplus 0 Area-deficit-intensity characteristics of drought by Norio Tase 0. Stachastic structure of water use time series by Jose D. Dalas -LaCruz and V. Yevjevich Gratis Area time structure of the monthly precipitation process by ich and Alan K. Karplus Gratis Area -deficit -intensity characteristics of.
Journal of Hydrology, 46 () Elsevier Scientific Publishing Company, Amsterdam -- Printed in The Netherlands [s] REGIONAL DROUGHT AND FLOOD FREQUENCY ANALYSIS: THEORETICAL CONSIDERATION ZEKAI ~EN* Civil Engineering Faculty, Department of Hydraulics and Water Power, Istanbul Technical University, Istanbul (Turkey) (Received August 1, ; accepted for Cited by: Area-time structure of the monthly precipitation process.
Jan ; 64; V Yevjevich; A K Karplus; Yevjevich, V., and Karplus, A. Area-time structure of the monthly precipitation process. Mathematical models for time series of monthly precipitation and monthly runoff, Hydrology papers (Colorado State University); no.
Yevjevich, V.M., An objective approach to definitions and investigations of continental hydrologic droughts. Abstract. The detection and measurement of precipitation by radar has been pursued since its introduction as a meteorological tool. The main advantage of using radar for precipitation estimation is that measurements can be made over large areas, with either fairly high temporal and spatial resolution or extensive spatial coverage (about 10 km 2 for ground-based radars and an order of Cited by: Drought monitoring needs comprehensive and integrated meteorological and hydrologic data.
However, such data are generally not available in extensive catchments. The present study aimed to analyze drought in the central plateau catchment of Iran using the terrestrial water storage deficit index (TSDI).
In this arid catchment, the meteorological and hydrologic observed data are : Ahmad Nemati, Seyed Hossein Ghoreishi Najafabadi, Gholamreza Joodaki, S. Saeid Mousavi Nadoushani. Monthly observed precipitation data (–) for five stations near the Hulun Lake are employed in this analysis to evaluate the applicability of satellite derived precipitation in study area.
Cited by: 4. Effective recharge from precipitation prooabiy can occur or.!-:n % few distant pitices, such cs at the base of the east slope of tac Wot Hills.
The interception of most of the precipitation by the pavement and buildings probably explains the luck of nse in water level in wcil lX/It.N'l after periods of heavy mm tail.
Catherine D. Neish, Lynn M. Carter, in Encyclopedia of the Solar System (Third Edition), Orbit Determination and the Yarkovsky Effect. Radar observations of NEAs can be used to reduce the uncertainty in an asteroid's orbital parameters by many orders of magnitude.
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Environmental Protection Agency Office of. Precipitation applied to the watershed model is uniform spatially, but varies with time. For complete drainage of the area, time for overland flow, channel flow, and storage must be considered. ordinates from each resulting hydrograph are summed to produce the total runoff hydrograph for the watershed.
This process is shown graphically. The purpose of this work is to estimate sampling errors of area-time averaged rain rate due to temporal samplings by satellites. In particular, the sampling errors of the proposed low inclination orbit satellite of the Tropical Rainfall Measuring Mission (TRMM) (35 deg inclination and km altitude), one of the sun synchronous polar orbiting satellites of NOAA series ( deg inclination.
Suggested Citation:"7 The Role of Monitoring and Modeling."National Research Council. Clean Coastal Waters: Understanding and Reducing the Effects of Nutrient gton, DC: The National Academies Press. doi: / -GPP: Amount of light energy converted to chemical energy (organic compounds) by autotrophs in an ecosystem during a given time period (energy/area/time: grams of carbon/m2/year) -NPP: The gross primary production of an ecosystem minus the energy used by the producers for respiration; the earth's energy budget; ~ billion tons of organic.
Development of Hydroinformatics in Thailand. Gebremichael, M. and W.F. Krajewski, Modeling distribution of temporal sampling errors in area-time averaged satellite rainfall estimates, Atmospheric Research, 73,Habib, E. G.J. Ciach and W.F. Krajewski, A method for filtering out raingauge representativeness errors from the verification distributions of radar and raingauge.This loss of coldness has impacted regional snow cover through a greater proportion of precipitation falling as rain or sleet instead of snow (Huntington et al.Feng and Hu ) and has resulted in earlier snowmelt (Hodgkins et al.Hodgkins and DudleyMatonse et al.Zion et al.Pradhanang et al.
).Cited by: 4.Nutrient limitation 2 is a basic concept of integrative biology, beginning inside the cell and scaling up to ecosystems. Consider the Droop equation (Droop ), designed to model growth rate of a single cell μ = μ m (1 − q / Q).
Here, μ is the biomass growth rate (day −1), μ m is the maximum growth rate at theoretically infinite quota, q is the minimum quota of a nutrient necessary Cited by: