Influence of high latitude anomalies on tropical climate phenomena and global climate

The tropical ocean and atmosphere are a highly active and very important region of the globe. Climate phenomena such as El Ni˜no (Philander, 1990), the Tropical Atlantic Dipole, and the Indian Ocean Dipole, play an important role in global climate variability. The tropical atmospheric boundary layer is very sensitive to even small changes in the sea surface temperature (SST). Small SST anomalies in the tropics can lead to shifts in the large scale convection cells and result in atmospheric heating. There is potential for positive feedback between the tropical ocean and atmosphere.Ocean waves are capable of propagating long distances very fast. Barotropic waves (adjustments in free surface height) can propagate round the globe within days. Baroclinic waves, propagating along the thermocline are able to cross the equatorial Atlantic in 2 – 3 months. This work shows the potential for ocean wave propagation to influence global climate, by linking high latitude anomalies to tropical climate phenomena.The first part of this thesis is a detailed examination of the “Tropical Atlantic Dipole” (TAD). Analysis of model data shows a dipole pattern in the SST, with strong cross-equatorial asymmetry in the surface mixed layer. Below the mixed layer the pattern becomes symmetric, and Kelvin and Rossby wave like adjustment can be seen to occur. However, the timeseries is not sufficiently long to provide confidence in resolving the power spectrum, and as such the results are inconclusive. The complexity of the model makes it difficult to identify the mechanism(s) which are responsible for driving the dipole. An idealised basin model is used to examine high latitude anomalies which create equatorward propagating coastal Kelvin waves as a possible driving mechanism for the TAD. The results show that coastal Kelvin wave propagation can quickly transmit a signal from the high latitude anomaly to the equator, and equatorial Kelvin and Rossby wave propagation can quickly influence the entire tropical ocean. This suggests that forcing of the TAD may come from higher latitudes, although it is still not fully understood how a symmetric sub-surface signal can become asymmetric at the surface. Restoring surface boundary conditions limit the response of the model, restricting the formation of a TAD. A similar experiment, using an idealised coupled model configuration is suggested, but not possible in the time available.The second part of this thesis looks in detail at the role of the ocean in rapidly transmitting a high latitude response to the equator, using an existing coupled climate model configured with realistic land geometry and bottom topography. Simulations of a salinity anomaly in the Southern Ocean show that it is possible to create an equatorial response in SST within a month, with SST anomalies of 2.5± after 6 months. Barotropic Kelvin and Rossby wave propagation is shown to be important in creating such a rapid equatorial response. Two points that are identified from this experiment are examined in further detail using an idealised basin model. Firstly, a mechanism for energy exchange within the equatorial waveguide is tested. Results suggest that it is not the mechanism responsible for the signals seen in the coupled climate model. Secondly, idealised model integrations confirm that transmission of signals along topographic ridges is possible. Signals strong enough to excite equatorward coastal Kelvin wave propagation are able to use topography to cross the Southern Ocean and reach the coast of Australia

pH-triggered phase inversion and separation of hydrophobised bacterial cellulose stabilised Pickering emulsions

The pH-triggered transitional phase behaviour of Pickering emulsions stabilised by hydrophobised bacterial cellulose (BC) is reported in this work. Neat BC was esterified with acetic (C2–), hexanoic (C6–) and dodecanoic (C12–) acids, respectively. We observed that C6– and C12–BC stabilised emulsions exhibited a pH-triggered reversible transitional phase separation. Water-in-toluene emulsions containing of 60 vol.% dispersed phase stabilised by C6– and C12–BC were produced at pH 5. Lowering the pH of the aqueous phase to 1 did not affect the emulsion type. Increasing the pH to 14, however, caused the emulsions to phase separate. This phase separation was caused by electrostatic repulsion between modified BC due to dissociable acidic surface groups at high pH, which lowered the surface coverage of the water droplets by modified BC. When the pH was re-adjusted to 1 again, w/o emulsions re-formed for C6– and C12–BC stabilised emulsions. C2–BC stabilised emulsions, on the other hand, underwent an irreversible pH-triggered transitional phase separation and inversion. This difference in phase behaviour between C2–BC and C6–/C12–BC was attributed to the hydrolysis of the ester bonds of C2–BC at high pH. This hypothesis is in good agreement with the measured degree of surface substitution (DSS) of modified BC after the pH-triggered experiments. The DSS of C2–BC decreased by 20% whilst the DSS remained constant for C6– and C12–BC

Surface functionalisation of bacterial cellulose as the route to produce green polylactide nanocomposites with improved properties

The effect of surface functionalisation of bacterial cellulose nanofibrils (BC) and their use as reinforcement for polylactide (PLLA) nanocomposites was investigated. BC was functionalised with various organic acids via an esterification reaction. This rendered the otherwise hydrophilic BC hydrophobic and resulted in better compatibility (interfacial adhesion) between PLLA and BC. A direct wetting method, allowing the determination of the contact angle of polymer droplets on a single BC nanofibre, was developed to quantify the interfacial adhesion between PLLA and functionalised BC. It was found that the contact angle between PLLA droplets and functionalised BC decreased with increasing chain lengths of the organic acids used to hydrophobise BC. A novel method to compound BC with PLLA based on thermally induced phase separation (TIPS) to yield a dry form of pre-extrusion composite was also developed. The mechanical properties of the surface functionalised BC reinforced PLLA nanocomposites showed significant improvements when compared to neat PLLA and BC reinforced PLLA. The thermal degradation and viscoelastic behaviour of the nanocomposites were also improved over neat PLLA

Efficacy of Cognitive and Metacognitive Interventions on Executive Functioning Post Traumatic Brain Injury to Enhance Occupational Performance

Cognitive rehabilitation (CR) is proposed as an effective intervention for individuals post Traumatic Brain Injury (TBI), by addressing cognitive function through remediating skills and practicing new compensatory skills. While there is considerable research, including systematic reviews that explore cognitive interventions post TBI, more research is needed in which occupational performance is the primary outcome of cognitive intervention. This current systematic review aims to synthesize the current body of evidence available on how using CR techniques to address executive functioning impact occupational performance in individuals who sustained a mild or moderate TBI

Non-paretic Forelimb Training Does Not Interfere with Recovery of Paretic Forelimb Strength After Experimental Middle Cerebral Artery Occlusion

Humans often compensate with their unimpaired (non-paretic) forelimb after surviving a stroke. Research in rats suggests that this can be maladaptive after focal motor cortical strokes. Forelimb weakness is understudied in rodent models of stroke. The purpose of the study is to determine whether behavioral experience with the non-paretic forelimb differentially affects paretic forelimb strength recovery after ischemic injury caused by middle cerebral artery occlusion (MCAo). Because behavioral manipulations can influence patterns of neural connectivity post-stroke, the present study also examined how training with non-paretic limb influenced corticostriatal projections. After training to proficiency with the preferred forelimb on the Isometric Pull Task, rats underwent MCAo in the hemisphere contralateral to this limb. One week after MCAo, rats were probed for initial impairment level and then assigned to either Non-Paretic Limb Training (NPT) or non-training control conditions for 14 days. Paretic limb performance was probed one day later. All rats then received six weeks of Rehabilitative Training (RT). The anterograde tract tracer BDA was then injected into the lesioned hemisphere. Training with the non-paretic limb (NPT) does not interfere with paretic limb recovery on the Isometric Pull Task, increase reliance on the impaired forelimb, or influence ipsi corticostriatal axon quantities after MCAo. Compensatory use of the non-paretic forelimb after strokes involving subcortical damage or cortical damage primarily in the somatosensory region may not be maladaptive for strength. Understanding how behavioral recovery varies with lesion locus could influence clinical management of patients

The North Atlantic subpolar circulation in an eddy-resolving global ocean model

The subpolar North Atlantic represents a key region for global climate, but most numerical models still have well-described limitations in correctly simulating the local circulation patterns. Here, we present the analysis of a 30-year run with a global eddy-resolving (1/12°) version of the NEMO ocean model. Compared to the 1° and 1/4° equivalent versions, this simulation more realistically represents the shape of the Subpolar Gyre, the position of the North Atlantic Current, and the Gulf Stream separation. Other key improvements are found in the representation of boundary currents, multi-year variability of temperature and depth of winter mixing in the Labrador Sea, and the transport of overflows at the Greenland–Scotland Ridge. However, the salinity, stratification and mean depth of winter mixing in the Labrador Sea, and the density and depth of overflow water south of the sill, still present challenges to the model. This simulation also provides further insight into the spatio-temporal development of the warming event observed in the Subpolar Gyre in the mid 1990s, which appears to coincide with a phase of increased eddy activity in the southernmost part of the gyre. This may have provided a gateway through which heat would have propagated into the gyre's interior

PKA-Dependent Phosphorylation of Serum Response Factor Inhibits Smooth Muscle-Specific Gene Expression

Our goal was to identify phosphorylation sites that regulate serum response factor (SRF) activity to gain a better understanding of the signaling mechanisms that regulate SRF’s involvement in smooth muscle cell (SMC)-specific and early response gene expression

Full-depth temperature trends in the Northeastern Atlantic through the early 21st century

The vertical structure of temperature trends in the northeastern Atlantic (NEA) is investigated from a blend of Argo and hydrography data. The representativeness of sparse hydrography sampling in the basin-mean is assessed using a numerical model. Between 2003 and 2013, the NEA underwent a strong surface cooling (0-450?m) and a significant warming at intermediate and deep levels (1000?m-3000?m) that followed a strong cooling trend observed between 1988 and 2003. During 2003-2013, gyre-specific changes are found in the upper 1000?m (warming and cooling of the subtropical and subpolar gyres, respectively) whilst the intermediate and deep warming primarily occurred in the subpolar gyre, with important contributions from isopycnal heave and water mass property changes. The full-depth temperature change requires a local downward heat flux of 0.53?±?0.06?W?m?2 through the sea-surface, and its vertical distribution highlights the likely important role of the NEA in the recent global warming hiatus

Octreotide and hepatocellular carcinoma

[No abstract available

Major variations in subtropical North Atlantic heat transport at short (5 day) timescales and their causes

Variability in the North Atlantic ocean heat transport at 26.5°N on short (5-day) timescales is identified and contrasted with different behaviour at monthly intervals using a combination of RAPID/MOCHA/WBTS measurements and the NEMO-LIM2 1/12° ocean circulation/sea ice model. Wind forcing plays the leading role in establishing the heat transport variability through the Ekman transport response of the ocean and the associated driving atmospheric conditions vary significantly with timescale. We find that at 5-day timescales the largest changes in the heat transport across 26.5°N coincide with north-westerly airflows originating over the American land mass that drive strong southward anomalies in the Ekman flow. During these events the northward heat transport reduces by 0.5-1.4 PW. In contrast, the Ekman transport response at longer monthly timescales is smaller in magnitude (up to 0.5 PW) and consistent with expected variations in the leading mode of North Atlantic atmospheric variability, the North Atlantic Oscillation. The north-westerly airflow mechanism can have a prolonged influence beyond the central 5-day timescale and on occasion can reduce the accumulated winter ocean heat transport into the North Atlantic by ∼40%