1,723,167 research outputs found
Clarke, D J, VX56592
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/377426Surname: CLARKE
Given Name(s) or Initials: D J
Military Service Number or Last Known Location: VX56592
Missing, Wounded and Prisoner of War Enquiry Card Index Number: 29783191244
Item: [2016.0049.09728] "Clarke, D J, VX56592
Clarke, D J, VX16708
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/377412Surname: CLARKE
Given Name(s) or Initials: D J
Military Service Number or Last Known Location: VX16708
Missing, Wounded and Prisoner of War Enquiry Card Index Number: 3569191230
Item: [2016.0049.09714] "Clarke, D J, VX16708
The role of irrigation models in European agriculture : investigating the impact of climate change
No full text
Climate impacts on groundwater in a UK coastal wetland
No full textGroundwater levels fundamentally control wetland environments and in dune systems groundwater levels are driven by the dynamics of seasonal, inter annual and longer term climatic conditions. Inter annual variations in these systems can be large and are often incorrectly attributed to climatic change. In this paper we present a 40 year record of groundwater levels and compare observed inter annual variations with estimates of the effects of anticipated climate chang
Predicted effects of climate change and sea level rise on water table levels and dune slack habitats
No full textSlack floors in dune systems are important for biodiversity, but are dynamic in their characteristics, both spatially and in time. Slack floors can be characterised as dry, partly wet or flooded, depending on the water table levels and in each case they can support differing vegetation and animal species. This paper examines the effects of changes in water table levels on the location of wet slack floors in the Aindsale NNR. A groundwater model is used to calculate the water table levels on a month by month basis based on climatic, hydrological and vegetation conditions. Detailed topographic survey data at 2m grid intervals from LIDAR imagery are used to represent the ground surface in the slack floors. The expected slack type (dry, damp, flooded) is generated by intersecting the LIDAR digital terrain model with the predicted water table levels. The model has been used to calculate the distribution and frequency of occurrence of the various slack floor types between 1972 and 2004. The UKCIP’02 climate change predictions have been used to estimate the future extent and size of flooded slack floors at Ainsdale up to the year 2100
Surface & Satellite techniques for irrigation monitoring & management
No full textAn overview of the current state of the art in research on water resources in the Aral Basi
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