scholarly journals Changes in Climatic Water Availability and Crop Water Demand for Iraq Region

2020 ◽  
Vol 12 (8) ◽  
pp. 3437 ◽  
Author(s):  
Saleem A. Salman ◽  
Shamsuddin Shahid ◽  
Haitham Abdulmohsin Afan ◽  
Mohammed Sanusi Shiru ◽  
Nadhir Al-Ansari ◽  
...  
Keyword(s):  
Climate Change ◽  
Water Availability ◽  
Water Demand ◽  
Early Period ◽  
Irrigated Agriculture ◽  
Rank Test ◽  
Crop Water ◽  
The North ◽  
Mk Test ◽  
Crop Water Demand

Decreases in climatic water availability (CWA) and increases in crop water demand (CWD) in the background of climate change are a major concern in arid regions because of less water availability and higher irrigation requirements for crop production. Assessment of the spatiotemporal changes in CWA and CWD is important for the adaptation of irrigated agriculture to climate change for such regions. The recent changes in CWA and CWD during growing seasons of major crops have been assessed for Iraq where rapid changes in climate have been noticed in recent decades. Gridded precipitation of the global precipitation climatology center (GPCC) and gridded temperature of the climate research unit (CRU) having a spatial resolution of 0.5°, were used for the estimation of CWA and CWD using simple water balance equations. The Mann–Kendall (MK) test and one of its modified versions which can consider long-term persistence in time series, were used to estimate trends in CWA for the period 1961–2013. In addition, the changes in CWD between early (1961–1990) and late (1984–2013) periods were evaluated using the Wilcoxon rank test. The results revealed a deficit in water in all the seasons in most of the country while a surplus in the northern highlands in all the seasons except summer was observed. A significant reduction in the annual amount of CWA at a rate of −1 to −13 mm/year was observed at 0.5 level of significance in most of Iraq except in the north. Decreasing trends in CWA in spring (−0.4 to −1.8 mm/year), summer (−5.0 to −11 mm/year) and autumn (0.3 to −0.6 mm/year), and almost no change in winter was observed. The CWA during the growing season of summer crop (millet and sorghum) was found to decrease significantly in most of Iraq except in the north. The comparison of CWD revealed an increase in agricultural water needs in the late period (1984–2013) compared to the early period (1961–1990) by 1.0–8.0, 1.0–14, 15–30, 14–27 and 0.0–10 mm for wheat, barley, millet, sorghum and potato, respectively. The highest increase in CWD was found in April, October, June, June and April for wheat, barley, millet, sorghum and potato, respectively.

Impact of climate change on surface water availability and crop water demand for the sub-watershed of Abbay Basin, Ethiopia

2019 ◽  
Vol 5 (4) ◽  
pp. 1859-1875 ◽  
Author(s):  
Alemu Ademe Bekele ◽  
Santosh Murlidhar Pingale ◽  
Samuel Dagalo Hatiye ◽  
Alemayehu Kasaye Tilahun
Keyword(s):  
Climate Change ◽  
Surface Water ◽  
Water Availability ◽  
Water Demand ◽  
Crop Water ◽  
Impact Of Climate Change ◽  
Crop Water Demand

scholarly journals Historical trends in Crop Water demand over Semi-Arid region of Syria

2021 ◽  
Author(s):  
Rajab Homsi ◽  
Shamsuddin Shahid ◽  
Zafar Iqbal ◽  
Atif Muhammad Ali ◽  
Ghaith Falah Ziarh
Keyword(s):  
Climate Change ◽  
Water Demand ◽  
Agricultural Production ◽  
Potential Evapotranspiration ◽  
Crop Water ◽  
Historical Trends ◽  
Climate Change Effects ◽  
The North ◽  
Crop Water Demand ◽  
Semi Arid Region

Abstract Climate change has caused a shift in aridity, particularly in the dry regions of the world which may subsequently affect several sectors predominantly the agricultural and water resources. This research examined the climate change effects on crop water demand (CWD) in Syria over the period 1951–2010. Given the lack of observed data, this analysis relied on (GPCC) precipitation and (CRU) temperature data from 1951 to 2010. Potential Evapotranspiration (PET) at each grid was calculated using Penman-Monteith method and FAO-56 model was used to calculate the crop water demand (CWD). The analysis revealed that CWD in Syria increased from 1981 to 2010 when compared to 1951–1980.The increase in CWD has been found for all the crops except wheat, whereas the maximum changes are found during April, and May. The differences in CWD for Barley between the two periods were found to be in the range of -20 to 40 mm. A decrease in CWD observed in the south of the country. However, a rise in 0 to 20 mm range was also discovered in the north. The CWD for wheat was found to decline in most parts of the country. However, it was found to increase in the north. The increase in CWD for barley and wheat has increased agricultural water stress in the region. Several agriculture planning needs to be developed in accordance with the expected future climate changes in order to maintain the agricultural production in the region.

IMPACT OF CLIMATE CHANGE ON CROP WATER DEMAND IN THE OKANAGAN VALLEY, B.C., CANADA

2004 ◽  
pp. 273-278
Author(s):  
D. Neilsen ◽  
C.A.S Smith ◽  
G. Frank ◽  
W.O. Koch ◽  
P. Parchomchuk
Keyword(s):  
Climate Change ◽  
Water Demand ◽  
Crop Water ◽  
Impact Of Climate Change ◽  
Crop Water Demand ◽  
Okanagan Valley

Future water supply and demand in the Peruvian Andes: assessment and implications

2020 ◽  
Author(s):  
Andrew J. Wade ◽  
Harvey J.E. Rodda ◽  
Nicholas P. Branch ◽  
Marcos Bruzzone ◽  
Alex Herrera ◽  
...  
Keyword(s):  
Climate Change ◽  
Water Supply ◽  
Water Demand ◽  
Supply And Demand ◽  
Local Communities ◽  
Dry Season ◽  
Adaptation Strategies ◽  
Crop Water ◽  
Peruvian Andes ◽  
Crop Water Demand

<p>The aim of the ACCESS project is to help assess the impact of climate change on socio-economic development in the Peruvian Andes, focused on the Ancash region, and to help identify adaptation strategies. As part of this larger effort, we are aiming to understand how climate change will impact: water availability and quality; farming, lives and livelihoods; and to work with local communities to plan adaptation strategies. The current water supply and demand in two catchments in the Cordillera Blanca and two in the Cordillera Negra is being assessed to understand the background water context in contrasting glaciated and non-glaciated landscapes. Based on detailed surveys of the ancient and modern waterscapes led by South American archaeologists, supplemented by more recent data from hydrological measurement and ethnographic surveys and discussions with local communities, a nuanced picture is emerging of how communities have adapted to past and current climate conditions, and potential solutions are being co-developed with the local communities to maintain and improve livelihoods in situations with low rainfall in the Negra and glacial retreat in the Blanca. Crop water demand during the dry season in the Rio Ancash (114 km<sup>2</sup>) catchment has been assessed using the CROPWAT model and local climate and crop survey data, and the present-day water supply assessed through the gauging of rivers and irrigation canal flows, and measurement of water quality and isotopes. Preliminary results, for the Rio Ancash, suggest the amount of water available for dry season irrigation on the mid-slopes is approximately 70 mm over the cropped area (57 km<sup>2</sup>) which appears to be less than the crop water demand, though this estimate may change as more data is processed. Initial climate projections suggestion an increase in water as the glaciers melt until around 2050. The dry season crop water demand and supply beyond 2050 is currently being estimated.</p>

scholarly journals GIS միջավայրում ոռոգման ջրի պահանջի հիմնավորումը կլիմայի փոփոխության պայմաններում

2021 ◽  
pp. 9-15
Author(s):  
A. G. Yeghiazaryan ◽  
P. S. Efendyan ◽  
G. M. Yeghiazaryan ◽  
L. G. Tovmasyan
Keyword(s):  
Climate Change ◽  
Water Demand ◽  
Water Source ◽  
Climatic Conditions ◽  
Cereal Crops ◽  
Crop Water ◽  
Spatial Changes ◽  
Crop Water Demand ◽  
Maximum Water ◽  
Gis Environment

The studies in GIS environment have been conducted on the example of Lori region. The investigations are based on the spatial changes of irrigation zones and agro-climatic conditions of Armenia. During the research, irrigation water and crop water demand has been estimated in the following climate change conditions: T +2° C and 0.9 P (T - estimated air temperature, P - atmosphertic precipitations). In case of 5 %, 25 %, 50 %, 75 % and 95 % atmospheric precipitations the water intake from water source has been changed. Maximum water requirement for vegetable and cereal crops, as well as for perennial plantations per irrigation zones has been forecasted.

scholarly journals Water Quality Threats, Perceptions of Climate Change and Behavioral Responses among Farmers in the Ethiopian Rift Valley

Climate ◽  
2021 ◽  
Vol 9 (6) ◽  
pp. 92
Author(s):  
Tewodros R. Godebo ◽  
Marc A. Jeuland ◽  
Christopher J. Paul ◽  
Dagnachew L. Belachew ◽  
Peter G. McCornick
Keyword(s):  
Climate Change ◽  
Water Quality ◽  
Surface Water ◽  
Water Availability ◽  
Agricultural Sector ◽  
Local Development ◽  
Irrigated Agriculture ◽  
Ethiopian Rift ◽  
Adaptation Mechanism ◽  
Main Ethiopian Rift

This work aims to assess water quality for irrigated agriculture, alongside perceptions and adaptations of farmers to climate change in the Main Ethiopian Rift (MER). Climate change is expected to cause a rise in temperature and variability in rainfall in the region, reducing surface water availability and raising dependence on groundwater. The study data come from surveys with 147 farmers living in the Ziway–Shala basin and water quality assessments of 162 samples from groundwater wells and surface water. Most groundwater samples were found to be unsuitable for long term agricultural use due to their high salinity and sodium adsorption ratio, which has implications for soil permeability, as well as elevated bicarbonate, boron and residual sodium carbonate concentrations. The survey data indicate that water sufficiency is a major concern for farmers that leads to frequent crop failures, especially due to erratic and insufficient rainfall. An important adaptation mechanism for farmers is the use of improved crop varieties, but major barriers to adaptation include a lack of access to irrigation water, credit or savings, appropriate seeds, and knowledge or information on weather and climate conditions. Local (development) agents are identified as vital to enhancing farmers’ knowledge of risks and solutions, and extension programs must therefore continue to promote resilience and adaptation in the area. Unfortunately, much of the MER groundwater that could be used to cope with declining viability of rainfed agriculture and surface water availability, is poor in quality. The use of saline groundwater could jeopardize the agricultural sector, and most notably commercial horticulture and floriculture activities. This study highlights the complex nexus of water quality and sufficiency challenges facing the agriculture sector in the region, and should help decision-makers to design feasible strategies for enhancing adaptation and food security.

Future Climatic Patterns and Sustainability of Current Cropping Patterns in a Water-Scarce River Basin of Eastern India 

2021 ◽  
Author(s):  
Smaranika Mahapatra ◽  
Madan Kumar Jha
Keyword(s):  
Water Demand ◽  
Agricultural Sector ◽  
Monsoon Rainfall ◽  
Baseline Period ◽  
Eastern India ◽  
Crop Water ◽  
Cropping Patterns ◽  
Water Demands ◽  
Crop Water Demand ◽  
Water Scarce

<p>Agricultural sector, being the largest consumer of water is greatly affected by climatic variability and disasters. Most parts of the world already face an enormous challenge in meeting competitive and conflicting multi-sector water demands. Climate change has further exacerbated this challenge by putting the sustainability of current cropping patterns and irrigation practices in question. For ensuring climate-resilient food production, it is crucial to examine the patterns of the projected climate and potential impacts on the agricultural sector at a basin scale. Hence, this study was carried out for an already water-scarce basin, Rushikulya River basin (RRB), located in the coastal region of eastern India. The bias-corrected NorESM2-MM general circulation model of Coupled Model Intercomparison Project-6 (CMIP6) was used in this study under four shared socioeconomic pathway (SSPs) scenarios, namely SSP126, SSP245, SSP370 and SSP585. The projected climatic parameters and crop water demands of the basin were analyzed assuming existing cropping pattern in the future. Analysis of the results reveals a significant and rapid increase in the temperature at a rate of 0.02-0.5ºC/year during 2026-2100 under all SSPs except SSP126, whereas the rainfall is expected to increase slightly during 2026-2100 as compared to the baseline period (1990-2016), especially in the far future (2076-2100) under all the SSPs. In contrast, monsoon rainfall is predicted to decrease under SSP245 and SSP370, while a slight increase in the monsoon rainfall is evident under SSP126 and SSP585. Although the rainy days will decrease slightly in the future 25-year time window, the number of heavy rainfall events is predicted to increase by two to three times. Also, retrospective analysis of rainfall and evapotranspiration suggested an existence of rainfall deficit (rainfall-evapotranspiration) in the basin throughout the year, except during July to September. The rainfall deficit in the basin during 2026-2100 is found to remain more or less same in the non-monsoon season, except for the month of October under SSP245, SSP370 and SSP585 scenarios where deficit increases by two folds. Rainfall is expected to be in surplus by 4 to 5 times higher under all SSPs except for SSP245. As to the evapotranspiration, an insignificant increasing trend is observed under future climatic condition with only 2 to 4% rise in the crop water demand compared to the baseline period. As the basin is already water stressed during most months in a year under baseline and future climatic conditions, continuing the current practice of monsoon paddy dominant cultivation in the basin will further aggravate this situation. The results of this study will be helpful in formulating sustainable irrigation plans and adaptation measures to address climate-induced water stress in the basin.</p><p><strong>Keywords:</strong> Climate change; CMIP6; SSP; Monsoon rainfall; Temperature; Crop water demand.</p>

scholarly journals DEMANDA HÍDRICA DO MARACUJAZEIRO AMARELO (Passiflora edulis Sims f. flavicarpa Deg.)

Irriga ◽  
2002 ◽  
Vol 7 (3) ◽  
pp. 185-190
Author(s):  
Ana Alexandrina Gama da Silva ◽  
Antonio Evaldo Klar
Keyword(s):  
Water Demand ◽  
Crop Coefficient ◽  
Passion Fruit ◽  
Crop Water ◽  
Passiflora Edulis ◽  
Crop Water Demand ◽  
Passiflora Edulis Sims ◽  
E Mail ◽  
Fruit Formation ◽  
Yellow Passion Fruit

DEMANDA HÍDRICA DO MARACUJAZEIRO AMARELO (Passiflora edulis Sims f. flavicarpa Deg.)   Ana Alexandrina Gama da SilvaEmbrapa Tabuleiros Costeiros, CP 44, CEP 49025-040, Aracaju, SE. E-mail: [email protected] Evaldo KlarDepartamento de Engenharia Rural, Faculdade de Ciências Agronômicas, Universidade Estadual Paulista, CP 237, CEP 18603-970, Botucatu, SP. E-mail: [email protected] Científico do CNPq   1 RESUMO  Determinou-se à demanda hídrica e o coeficiente de cultivo (Kc) do maracujá amarelo (Passiflora edulis Sims f. flavicarpa Deg.), seleção Sul-Brasil, cultivado sob irrigação localizada, no município de Botucatu-SP (22o 51’ S,  48o 26’ W). A evapotranspiração máxima da cultura (ETc) e a evapotranspiração de referência (ETo) foram medidas em lisímetros de nível de lençol freático constante, durante o período de 29 de setembro de 2000 a 20 de julho de 2001. Os valores da ETc e ETo foram de 954,98 mm e  1.069,21 mm, respectivamente, durante todo o período medido. Os valores de Kc variaram de 0,42 a 1,12, com os valores máximos registrados entre 150 e 210 dias após o transplantio das mudas no campo (DAT), período correspondente aos estádios fenológicos de florescimento e formação dos frutos.  UNITERMOS: Passiflora edulis, evapotranspiração, coeficiente de cultivo (Kc).   SILVA, A.A.G. da, KLAR, A.E.  YELLOW PASSION FRUIT (Passiflora edulis Sims f. flavicarpa Deg.) CROP: WATER DEMAND.   2 ABSTRACT  Crop water demand and crop water coefficient (Kc = ETc/ETo) of yellow passion fruit were evaluated in constant level lysimeters under drip irrigation from September 21, 2000 to July 31, 2001 in Botucatu-SP. The maximum crop water demand (ETc) and the Reference Evapotranspiration (ETo), measured by lysimeters, were 954.98 mm and 1,069.21 mm, respectively, during all period measured. The values of Kc varied from 0.42 to 1.12  with maximum values registered from 150 to 210 days following transplanting during flowering and fruit formation  phases.  KEYWORDS: Passiflora edulis, evapotranspiration, crop coefficient (Kc). 

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