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  <channel rdf:about="http://hdl.handle.net/1842/1637">
    <title>ERA Collection:</title>
    <link>http://hdl.handle.net/1842/1637</link>
    <description />
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        <rdf:li rdf:resource="http://hdl.handle.net/1842/6574" />
        <rdf:li rdf:resource="http://hdl.handle.net/1842/6506" />
        <rdf:li rdf:resource="http://hdl.handle.net/1842/6270" />
        <rdf:li rdf:resource="http://hdl.handle.net/1842/6247" />
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    <dc:date>2013-06-19T04:35:05Z</dc:date>
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  <item rdf:about="http://hdl.handle.net/1842/6574">
    <title>Understanding the effects of drought upon carbon allocation and cycling in an Amazonian rain forest</title>
    <link>http://hdl.handle.net/1842/6574</link>
    <description>Title: Understanding the effects of drought upon carbon allocation and cycling in an Amazonian rain forest
Authors: Metcalfe, Daniel Benjamin
Abstract: The Amazon rain forest plays an important role in regional and global&#xD;
biogeochemical cycling, but the region may undergo an increase in the frequency and&#xD;
severity of drought conditions driven by global climate change, regional deforestation&#xD;
and fire. The effects of this drought on carbon cycling in the Amazon, particularly&#xD;
below-ground, are potentially large but remain poorly understood. This thesis&#xD;
examines the impacts of seasonal and longer-term drought upon ecosystem carbon&#xD;
allocation and cycling at an Amazon rain forest site with a particular focus upon&#xD;
below-ground processes. Measurements are made at three one-hectare forest plots&#xD;
with contrasting soil type and vegetation structure, to observe responses across a&#xD;
range of Amazon primary forest types. A fourth plot is subjected to partial rainfall&#xD;
exclusion to permit measurement of forest responses to a wider range of soil moisture&#xD;
levels than currently exists naturally.&#xD;
An analysis of the number of samples required to accurately quantify important&#xD;
ecosystem carbon stocks and fluxes is used to guide the sampling strategy at the field&#xD;
site. Quantifying root dynamics, in particular, presents methodological challenges.&#xD;
Thus, I critically review existing methods, and develop techniques to accurately&#xD;
measure root standing biomass and production. Subsequently, these techniques are&#xD;
used to record root responses, in terms of standing biomass, production, morphology,&#xD;
turnover and nutrient content, to variation in soil moisture across the four rain forest&#xD;
plots. There is substantial environmental variation in root characteristics. However,&#xD;
several responses remain consistent across plots: root production of biomass, length,&#xD;
and surface area, is lower where soil is dry, while root length and surface area per unit&#xD;
mass show the opposite pattern.&#xD;
The other major component of the below-ground carbon cycle is soil carbon&#xD;
dioxide efflux. I partition this efflux, on each plot, into contributions from organic&#xD;
ground surface litter, roots and soil organic matter, and investigate abiotic and biotic causes for observed differences within and between plots. On average, the percentage&#xD;
contribution of soil organic matter respiration to total soil carbon dioxide efflux&#xD;
declines during the dry season, while root respiration contribution displays the&#xD;
opposite trend. However, spatial patterns in soil respiration are not directly&#xD;
attributable to variation in either soil moisture or temperature. Instead, ground surface&#xD;
organic litter mass and root mass account for 44 % of observed spatial heterogeneity&#xD;
in soil carbon dioxide efflux.&#xD;
Finally, information on below-ground carbon cycling is combined with aboveround&#xD;
data, of canopy dynamics and stem wood production and mortality, to analyze&#xD;
the potential effects of drought upon carbon cycling in an Amazon forest ecosystem.&#xD;
Comparison of the rainfall exclusion plot with a similar, but unmodified, control plot&#xD;
reveals potentially important differences in tree carbon allocation, mortality,&#xD;
reproduction, soil respiration and root dynamics. The apparent net consequence of&#xD;
these changes is that, under drier conditions, the amount of CO2 moving out of the&#xD;
forest and into the atmosphere is diminished. This synthesis of above-ground and&#xD;
below-ground data advances understanding of carbon cycling in rain forests, and&#xD;
provides information which should allow more accurate modelling of the response of&#xD;
the Amazon region to future drought. Additional measurements at other sites, and of&#xD;
other ecosystem carbon fluxes, should further refine modelling predictions.</description>
    <dc:date>2007-11-27T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/1842/6506">
    <title>Modelling the effects of genetic line and feeding system on methane emissions from dairy systems</title>
    <link>http://hdl.handle.net/1842/6506</link>
    <description>Title: Modelling the effects of genetic line and feeding system on methane emissions from dairy systems
Authors: Bell, Matthew
Abstract: Dairy cattle make a significant contribution to global methane emissions. Milking cows&#xD;
in the UK make up about a fifth of the total cattle population, with Holstein-Friesian&#xD;
cows being the most common breed. Investigating ways to minimise methane, a potent&#xD;
greenhouse gas (GHG) produced by dairy cows from enteric fermentation and manure,&#xD;
has gained importance in recent years due its role in climate change. Currently, GHG&#xD;
emissions from UK dairy farming are predicted using the Intergovernmental Panel on&#xD;
Climate Change (IPCC) Tier II methodology. The IPCC Tier II methodology and&#xD;
statistical prediction equations from the literature were evaluated for their ability to&#xD;
reliably model methane output using data from the Langhill Holstein-Friesian&#xD;
experimental herd. The Langhill dairy herd is on a long-term breeding and feeding&#xD;
systems experiment, and cows are on average 88% North American Holstein genes. The&#xD;
production systems within the herd represent a range of dairy systems that may be found&#xD;
commercially. Therefore, production values were assumed to be representative of those&#xD;
that could be found in the commercial Holstein-Friesian population, so factors affecting&#xD;
system methane emissions and appropriate mitigation options could be investigated.&#xD;
Prediction equations using dry matter (DM) intake and gross energy intake as input&#xD;
values were the most appropriate equations for reliably estimating daily enteric methane&#xD;
output. However, if DM intake values are not available, the IPCC Tier II method was&#xD;
found to provide a suitable prediction of methane emissions over a cow‘s lactation and&#xD;
lifetime. This study found that GHG emissions from enteric fermentation and manure,&#xD;
expressed as carbon dioxide equivalents (CO2-eq.), account for about 66% of dairy&#xD;
system CO2-eq. emissions, with enteric methane output being the main contributor (34%&#xD;
of system CO2-eq. emissions). Breeding for increased kilograms of milk fat plus protein&#xD;
production was shown to help reduce dairy system methane emissions. Cows of&#xD;
predominantly North American Holstein genes in this study produced more milk when&#xD;
fed a diet with a low proportion of forage and had lower GHG emissions and land&#xD;
requirement per kilogram energy corrected milk than similar cows fed a diet with a&#xD;
higher proportion of forage. Strategies to mitigate GHG emissions (including methane) and the environmental impact of dairy systems should seek to select animals that better&#xD;
utilise their feed intake to meet their genetic potential for milk production.</description>
    <dc:date>2011-06-28T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/1842/6270">
    <title>Using satellite remote sensing to quantify woody cover and biomass across Africa</title>
    <link>http://hdl.handle.net/1842/6270</link>
    <description>Title: Using satellite remote sensing to quantify woody cover and biomass across Africa
Authors: Mitchard, Edward Thomas Alexander
Abstract: The goal of quantifying the woody cover and biomass of tropical savannas, woodlands&#xD;
and forests using satellite data is becoming increasingly important, but limitations in&#xD;
current scientific understanding reduce the utility of the considerable quantity of satellite&#xD;
data currently being collected. The work contained in this thesis reduces this knowledgegap,&#xD;
using new field data and analysis methods to quantify changes using optical, radar&#xD;
and LiDAR data.&#xD;
The first paper shows that high-resolution optical data (Landsat &amp; ASTER) can be used&#xD;
to track changes in woody vegetation in the Mbam Djerem National Park in Cameroon.&#xD;
The method correlates a satellite-derived vegetation index with field-measured canopy&#xD;
cover, and the paper concludes that forest encroached rapidly into savanna in the region&#xD;
from 1986-2006. Using the same study area, but with radar remote sensing data from&#xD;
1996 and 2007 (ALOS PALSAR &amp; JERS-1), the second paper shows that radar&#xD;
backscatter correlates well with field-measured aboveground biomass (AGB). This&#xD;
dataset confirms the woody encroachment within the park; however, in a larger area&#xD;
around the park, deforestation dominates.&#xD;
The AGB-radar relationships described above are expanded in the next paper to include&#xD;
field plots from Budongo Forest (Uganda), the Niassa Reserve (north Mozambique), and&#xD;
the Nhambita Community Project (central Mozambique). A consistent AGB-radar&#xD;
relationship is found in the combined dataset, with the RMSE for predicted AGB values&#xD;
for a site increasing by &lt;30 %, compared with a site-specific equation, when using an&#xD;
AGB-radar equation derived from the three other sites. The study of the Nhambita site is&#xD;
extended in the following paper to assess the ability of radar to detect change over short&#xD;
time periods in this environment, as will be needed for REDD (Reducing Emissions&#xD;
from Deforestation and Degradation). Using radar mosaics from 2007 and 2009, areas&#xD;
known (from detailed ground data) to have been degraded decreased in AGB in the radar&#xD;
change detection, whereas areas of agroforestry and forest protection showed small&#xD;
increases.</description>
    <dc:date>2012-06-25T00:00:00Z</dc:date>
  </item>
  <item rdf:about="http://hdl.handle.net/1842/6247">
    <title>Satellite investigations of ice dynamics and supraglacial lake development in Greenland</title>
    <link>http://hdl.handle.net/1842/6247</link>
    <description>Title: Satellite investigations of ice dynamics and supraglacial lake development in Greenland
Authors: Briggs, Kate Hannah
Abstract: This thesis aims to improve the current understanding of the processes which control&#xD;
the flow variability of Greenland Ice Sheet (GrIS) outlet glaciers. The most recent&#xD;
Intergovernmental Governmental Panel on Climate Change (IPCC) report (Meehl et&#xD;
al., 2007) identifies that a critical limitation to forecasts of sea-level rise are&#xD;
uncertainties in modelling the ice dynamics of the GrIS. Using Synthetic Aperture&#xD;
Radar (SAR) feature tracking, seasonal velocities of land- and marine- terminating&#xD;
glaciers in a region in the northeast of Greenland are measured. Records of air&#xD;
temperature in conjunction with seasonal observations of supraglacial lake&#xD;
development, sea ice conditions and ice front positions, derived from SAR imagery,&#xD;
are used to investigate the controls on the observed variations in ice velocity. A clear&#xD;
link between ice velocities and glacier hydrology is found. These findings are&#xD;
consistent with observations from other glaciers in Greenland and are suggestive of a&#xD;
universal hydrological forcing of ice velocity for the whole of the GrIS ablation&#xD;
zone.&#xD;
Lake drainage events have been identified as a key factor in linking atmospheric&#xD;
changes, glacier hydrology and ice velocities in Greenland. For modelling purposes,&#xD;
a means of parameterising the distribution and evolution of supraglacial lakes is&#xD;
therefore needed. Assuming that water will pond in surface depressions, this thesis&#xD;
assesses the ability of using Digital Elevation Models (DEMs) for this purpose. High&#xD;
resolution DEMs are created using Interferometric SAR (InSAR) for two, separate&#xD;
regions of the GrIS. The positions and areal extent of surface depressions are&#xD;
compared with those of lakes observed in optical satellite imagery. The level of&#xD;
correspondence between the two datasets is found to be poor as a result of the&#xD;
resolution of the DEMs and the physical differences between surface depressions and&#xD;
lakes (e.g. lakes may not fill the capacity of the depression). An alternative method&#xD;
for parameterising the seasonal distribution of supra-glacial lakes, by extrapolating&#xD;
trends observed in current lake distributions, is investigated. The locations and&#xD;
evolution of lakes in the west of Greenland during the summer of 2003 are mapped&#xD;
using 47 Moderate Resolution Imaging Spectroradiometer (MODIS) images. Clear trends are identified in the distributions of lakes with elevation and are linked to the&#xD;
seasonal melt-cycle and to changes in ice thickness and its influence on surface&#xD;
depressions, tensile stresses and hydrofracturing. It may be possible to extrapolate&#xD;
these trends to other regions and higher elevations on the ice sheet, thereby enabling&#xD;
the distribution of lakes to be parameterised in ice sheet models. The findings of this&#xD;
thesis help to contribute to the understanding of the interaction between climate and&#xD;
ice dynamics in the context of the GrIS.</description>
    <dc:date>2012-06-25T00:00:00Z</dc:date>
  </item>
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