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51.
Climate links and recent extremes in antarctic sea ice, high-latitude cyclones, Southern Annular Mode and ENSO 总被引:2,自引:0,他引:2
In this article, we study the climate link between the Southern Annular Mode (SAM) and the southern sea-ice extent (SIE), and discuss the possible role of stationary waves and synoptic eddies in establishing this link. In doing so, we have used a combination of techniques involving spatial correlations of SIE, eddy streamfunction and wind anomalies, and statistics of high-latitude cyclone strength. It is suggested that stationary waves may be amplified by eddy anomalies associated with high latitude cyclones, resulting in more sea ice when the SAM is in its positive phase for most, but not all, longitudes. A similar association is observed during ENSO (La Ni?a years). Although this synergy in the SAM/ENSO response may partially reflect preferential areas for wave amplification around Antarctica, the short extent of the climate records does not allow for a definite causality connection to be established with SIE. Stronger polar cyclones are observed over the areas where the stationary waves are amplified. These deeper cyclones will break up and export ice equatorward more efficiently, but the near-coastal regions are cold enough to allow for a rapid re-freeze of the resulting ice break-up. We speculate that if global warming continues this same effect could help reverse the current (positive) Antarctic SIE trends once the ice gets thinner, similarly to what has been observed in the Northern Hemisphere. 相似文献
52.
A detailed hydrogeological and hydrochemical study was carried out in Yamuna-Krishni sub-basin which is a part of the vast
central Ganga plain. Groundwater is the major source of water supply for agricultural, domestic and industrial uses. The excess
use of groundwater has resulted in depletion of water levels. The groundwater quality, too, has deteriorated in areas dominated
by industrial activity. This has led to the preparation of a groundwater vulnerability map in relation to contamination. Groundwater
vulnerability maps are valuable derivative maps that show, quantitatively or qualitatively, certain characteristics of the
sub-surface environment that determine vulnerability of groundwater to contamination. The modified DRASTIC method was used
to prepare vulnerability map. The parameters like depth to water, net recharge, aquifer media, soil media, impact of vadose
zone, hydraulic conductivity and land use pattern, owing to its bearing on groundwater regime, were considered to prepare
vulnerability map. The vulnerability index is computed as the sum of the products of weight and rating assigned to each of
the input considered as above. The vulnerability index ranges from 140 to 180, and is classified into four classes i.e. 140–150,
150–160, 160–170 and 170–180 corresponding to low, medium, high and very high vulnerability zones respectively. Using this
index, a groundwater vulnerability potential map was generated which shows that 7%, 40% and 53% of the study area falls in
low, medium and high to very high vulnerability zones respectively. The map, thus generated, can be used as a tool for protection
and management of aquifers from contamination. 相似文献
53.
Hafiz Muhammad Awais Rashid J. A. D. K. Wanigarathna L. C. Kurukulasuriya N. H. Priyankara A. M. N. Alagiyawanna Takeshi Saito Ken Kawamoto 《Environmental Earth Sciences》2017,76(11):396
This study aimed to develop a low-cost and effective clay liner material for solid waste landfills in Sri Lanka. A locally available clayey soil and its admixtures with 5 and 10% bentonite were examined for this purpose. Laboratory experiments to determine soil plasticity and swell index were carried out on the tested samples. Hydraulic conductivity (k) tests were carried out in the laboratory using water and an aqueous solution of CaCl2 on unconsolidated samples prepared by either dry or slurry packing and pre-consolidated samples with five different consolidation pressures (p) from 10 to 200 kPa. Measured liquid limits for tested admixtures increased with increasing bentonite contents and correlated well with measured values of the swell index. The difference in permeant solutions had little effect on measured k values for both unconsolidated and pre-consolidated samples. The hydraulic conductivities were highly affected by changing p, i.e., the k values decreased on two orders of magnitude as p increased from 10 to 200 kPa. The Kozeny–Carman equation, a theoretical permeability model that expresses the k-porosity relationship, was applied to measured data including reported values. Results showed the Kozeny–Carman equation captured well the porosity-dependent k values for tested soils and their admixtures with bentonite under a wide range of void ratios, suggesting that the Kozeny–Carman equation is a useful tool to estimate the magnitude of k values for differently compacted soil and its bentonite admixtures. 相似文献
54.
This study records length-weight relationships(LWRs)for eleven commercially important marine catfi sh species of the family Ariidae(sea catfi shes)and Plotosidae(eel catfi shes)from the northern Arabian Sea coast of Pakistan.The specimens were sampled from December 2014 to November 2015,using bottom trawls with various mesh sizes by commercial vessels.The species were Nemapteryx caelatus,Sciades sona,Arius gagora,Batrachocephalus mino,Netuma thalassina,N.bilineata,Osteogeneiosus militaris,Plicofollis dussumieri,P.tenuispinis,Plotosus limbatus,and P.lineatus.Of the eleven species,two species A.gagora and N.bilineata were recorded for the fi rst time and LWRs for four species A.gagora,N.bilineata,S.sona,and B.mino still have no data in the Fish Base database.In addition,new maximum length for each of the three species N.bilineata,O.militaris and B.m ino was also found. 相似文献
55.
Groundwater flow modelling of Yamuna-Krishni interstream,a part of central Ganga Plain Uttar Pradesh 总被引:4,自引:0,他引:4
Groundwater is a major source of water for agricultural and domestic requirements in western Uttar Pradesh. Due to increasing
agricultural requirements the abstraction of groundwater has increased manifold in the last two-to-three decades. The quaternary
alluvium hosts the aquifer in the region. The study area forms a part of Yamuna-Krishni interfluve. Although the area hosts
potential aquifers these have been adversely affected by poor management. For effective groundwater management of a basin
it is essential that a careful water balance study should be carried out. Keeping this in mind groundwater flow modelling
was attempted to simulate the behaviour of the flow system and evaluate the water balance. The groundwater flow modelling
was carried out. The horizontal flows, seepage losses from unlined canals, recharge from rainfall and irrigation return flows
were applied using different boundary packages available in Visual MODFLOW, Pro 4.1. The river-aquifer interaction was simulated
using the river boundary package. Hydraulic conductivity values were applied to specific zones and these ranged from 9.8 to
26.6m/day. Recharge due to rainfall and irrigation returns were assigned to respective zones. Pumping rates of 500m3/day, 1000m3/day, 1500m3/day, 2000m3/day and 2500m3/day were applied to appropriate areas of the model to simulate areas of stress. The zone budget shows a water balance deficit
for the period June 2006 to June 2007. The total recharge to the study area is 160.21 million m3 (Mcum). The groundwater draft through pumping is of the order of 233.56 Mcum, thus leaving a deficit balance of −73.35 Mcum.
The sensitivity of the model to input parameters was tested by varying the parameters of interest over a range of values,
monitoring the response of the model and determining the root mean square error of the simulated groundwater heads to the
measured heads. These analyses showed that the model is most sensitive to hydraulic conductivity and recharge parameters.
Three scenarios were considered to predict aquifer responses under varied conditions of groundwater bstraction. 相似文献
56.
57.
Many studies such as climate variability, climate change, trend analysis, hydrological designs, agriculture decision-making etc. require long-term homogeneous datasets. Since homogeneous climate data is not available for climate analysis in Pakistan and India, the present study emphases on an extensive quality control and homogenization of daily maximum temperature, minimum temperature and precipitation data in the Jhelum River basin, Pakistan and India. A combination of different quality control methods and relative homogeneity tests were applied to achieve the objective of the study. To check the improvement after homogenization, correlation coefficients between the test and reference series calculated before and after the homogenization process were compared with each other. It was found that about 0.59%, 0.78% and 0.023% of the total data values are detected as outliers in maximum temperature, minimum temperature and precipitation data, respectively. About 32% of maximum temperature, 50% of minimum temperature and 7% of precipitation time series were inhomogeneous, in the Jhelum River basin. After the quality control and homogenization, 1% to 11% improvement was observed in the infected climate variables. This study concludes that precipitation daily time series are fairly homogeneous, except two stations (Naran and Gulmarg), and of a good quality. However, maximum and minimum temperature datasets require an extensive quality control and homogeneity check before using them into climate analysis in the Jhelum River basin. 相似文献
58.
59.
Glaciers are among the most conspicuous and dynamic features on the earth’s surface and are also highly sensitive to changes in climatic parameters. Glaciers in the Kashmir Himalayas have been reported to be retreating due to climate forcing. Kolahoi Glacier is one of the largest and important glaciers of the Kashmir Himalayas and is the main source of Liddar River, which is the largest tributary of the Jhelum River system. In the present study, an analysis to assess the response of Kolahoi Glacier to the changing climate was carried out using the Survey of India (SoI) map and multi-temporal Landsat satellite data. The results show a significant change in the spatial extent of Kolahoi Glacier. The total area of this glacier has reduced from 12.21 km2 in 1962 to 11.61 km2 in 2010. An analysis of meteorological data (temperature and precipitation) shows that the average annual temperature increased from 9.1 °C in 1980–1989 to 10.3 °C in 2000–2009, while the precipitation decreased from 1329.44 to 1126.89 mm during the same period. The results suggest that this glacier will be annihilated completely if the same retreating trend continues. 相似文献
60.
Bilal Rashid Astor-Lonice Bal Glyn J. J. Williams Ann H. Muggeridge 《Computational Geosciences》2012,16(2):409-422
The vorticity of the displacement velocity is used to derive dimensionless numbers that can be used to quantify the relative
importance of viscosity ratio, gravity, diffusion/dispersion and permeability heterogeneity on secondary hydrocarbon recovery.
Using this approach, a new objective measure of the impact of permeability and porosity heterogeneity on reservoir performance
is obtained. This is used, in conjunction with other dimensionless numbers, to analyse the relative impact of heterogeneity,
buoyancy effects, mobility ratio and dispersion on breakthrough time and recovery at 1 pore volume injected during first contact
miscible gas injection. This is achieved using results obtained from detailed simulation of miscible displacements through
a range of geologically realistic reservoir models. This study goes some way towards developing a unified mathematical framework
to determine under which flow conditions reservoir heterogeneity becomes more important than other physical processes. We
propose that comparison of these dimensionless numbers can be used to identify the key factors controlling recovery and thus
assist the engineer in determining appropriate enhanced oil recovery techniques to improve recovery. 相似文献