title: Book review: The Realist Hope: a Critique of Anti-Realist Approaches in Contemporary Philosophical Theology (Heythrop Studies in Contemporary Philosophical Theology). By Christopher J. Insole

authors: Walker, Ruth

subjects: book review

abstract: The article reviews the book “Book review: The Realist Hope: a Critique of Anti-Realist Approaches in Contemporary Philosophical Theology (Heythrop Studies in Contemporary Philosophical Theology)” by Christopher J. Insole.

text: Book review: The Realist Hope: a Critique of Anti-Realist Approaches in Contemporary Philosophical Theology (Heythrop Studies in Contemporary Philosophical Theology). By Christopher J. Insole The article reviews the book “Book review: The Realist Hope: a Critique of Anti-Realist Approaches in Contemporary Philosophical Theology (Heythrop Studies in Contemporary Philosophical Theology)” by Christopher J. Insole.

year: 2009

title: Effects of surfzone wave transformation on swash dynamics

authors: Guedes, Rafael Marcondes Carvalho

subjects: swash

abstract: Swash oscillations on two natural beaches were measured to show that the shape and magnitude of energy spectra can be largely dependent on processes occurring inside the surfzone. The observations took place on a steep, intermediate beach on the east coast (Tairua Beach), and a low-sloping, dissipative beach located on the west coast of New Zealand (Ngarunui Beach, Raglan), and aimed at improving the understanding of the effects of wave breaking, beach slope, and nonlinear wave interactions on the swash oscillations. These problems were addressed by analysing datasets obtained from field experiments undertaken at these two sites.
A field experiment at Tairua Beach showed that swash oscillations were critically dependent on the stage of the tide which controlled the degree of wave energy dissipation over the sandbar crest. Under mild, near-constant offshore wave conditions, the presence of a sandbar and the tidally-controlled water depth over its crest determined whether most of the incoming waves broke before reaching the shoreline. This forced a change in the pattern of wave energy dissipation across the surfzone between low and high tide, which was reflected by changes to swash elevation (runup) on time-scales of a few hours. Significant runup height Rs, defined as 4 times the standard deviation of the waterline time series, varied by a factor of 2 between low tide, when most of the waves were breaking over the sandbar and high tide, when the waves were barely breaking. The increase in wave energy dissipation during low tide was associated with changes in swash maxima distribution, decrease in mean swash period and increasing energy at infragravity frequencies (0.004–0.05 Hz). Bispectral analysis suggested this infragravity modulation might be connected with the presence of secondary waves at the shoreline.
Swash oscillations at Tairua were not homogeneous along the beach. Alongshore variability in Rs of up to 78% was observed and was mainly driven by changes in the sea-swell (0.05–0.4 Hz) band of the swash. This variability was predominantly controlled by alongshore changes in beach face slope, although alongshore patterning in wave breaking over the sandbar caused alongshore changes in wave dissipation and also resulted in alongshore swash variation in the sea-swell bandwidth. At infragravity frequencies, alongshore swash variability was not well associated either with changes in beach slope or wave breaking and was possibly linked to the presence of low-mode edge waves, observed from frequency-wavenumber spectra of the swash time series.
A final experiment was conducted to understand the surfzone control on incident and infragravity runup on a gently-sloping beach. The observations showed that runup saturation at infragravity frequencies can occur under mild offshore energy conditions if the beach slope is sufficiently gentle. Infragravity saturation was observed for higher-frequency (> 0.025–0.035 Hz) infragravity waves, where typically less than 5% of the (linear) energy flux was reflected from the beach and where, similar to the sea-swell band, the swash energy was independent of offshore wave energy. The infragravity frequency range of saturation was determined by the tide, with saturation extending to lower frequencies at low tide when the local beach face slope over the concave-shaped profile was gentler. Runup was strongly dominated by infragravity frequencies, which accounted on average for 96% of the runup variance, and its energy levels were entirely consistent with strong infragravity wave dissipation observed in the surfzone, particularly when including the nonlinear contributions to the wave energy fluxes. Our observations show evidence of nonlinear interactions involving infragravity and high-frequency, harmonic waves, and suggest that these harmonics could play a role in the wave energy balance near the shoreline on low-sloping, dissipative beaches.

text: Effects of surfzone wave transformation on swash dynamics Swash oscillations on two natural beaches were measured to show that the shape and magnitude of energy spectra can be largely dependent on processes occurring inside the surfzone. The observations took place on a steep, intermediate beach on the east coast (Tairua Beach), and a low-sloping, dissipative beach located on the west coast of New Zealand (Ngarunui Beach, Raglan), and aimed at improving the understanding of the effects of wave breaking, beach slope, and nonlinear wave interactions on the swash oscillations. These problems were addressed by analysing datasets obtained from field experiments undertaken at these two sites.
A field experiment at Tairua Beach showed that swash oscillations were critically dependent on the stage of the tide which controlled the degree of wave energy dissipation over the sandbar crest. Under mild, near-constant offshore wave conditions, the presence of a sandbar and the tidally-controlled water depth over its crest determined whether most of the incoming waves broke before reaching the shoreline. This forced a change in the pattern of wave energy dissipation across the surfzone between low and high tide, which was reflected by changes to swash elevation (runup) on time-scales of a few hours. Significant runup height Rs, defined as 4 times the standard deviation of the waterline time series, varied by a factor of 2 between low tide, when most of the waves were breaking over the sandbar and high tide, when the waves were barely breaking. The increase in wave energy dissipation during low tide was associated with changes in swash maxima distribution, decrease in mean swash period and increasing energy at infragravity frequencies (0.004–0.05 Hz). Bispectral analysis suggested this infragravity modulation might be connected with the presence of secondary waves at the shoreline.
Swash oscillations at Tairua were not homogeneous along the beach. Alongshore variability in Rs of up to 78% was observed and was mainly driven by changes in the sea-swell (0.05–0.4 Hz) band of the swash. This variability was predominantly controlled by alongshore changes in beach face slope, although alongshore patterning in wave breaking over the sandbar caused alongshore changes in wave dissipation and also resulted in alongshore swash variation in the sea-swell bandwidth. At infragravity frequencies, alongshore swash variability was not well associated either with changes in beach slope or wave breaking and was possibly linked to the presence of low-mode edge waves, observed from frequency-wavenumber spectra of the swash time series.
A final experiment was conducted to understand the surfzone control on incident and infragravity runup on a gently-sloping beach. The observations showed that runup saturation at infragravity frequencies can occur under mild offshore energy conditions if the beach slope is sufficiently gentle. Infragravity saturation was observed for higher-frequency (> 0.025–0.035 Hz) infragravity waves, where typically less than 5% of the (linear) energy flux was reflected from the beach and where, similar to the sea-swell band, the swash energy was independent of offshore wave energy. The infragravity frequency range of saturation was determined by the tide, with saturation extending to lower frequencies at low tide when the local beach face slope over the concave-shaped profile was gentler. Runup was strongly dominated by infragravity frequencies, which accounted on average for 96% of the runup variance, and its energy levels were entirely consistent with strong infragravity wave dissipation observed in the surfzone, particularly when including the nonlinear contributions to the wave energy fluxes. Our observations show evidence of nonlinear interactions involving infragravity and high-frequency, harmonic waves, and suggest that these harmonics could play a role in the wave energy balance near the shoreline on low-sloping, dissipative beaches.

year: 2012

title: Can te ao Māori worldviews exist within a western institute’s online teaching and learning environment?

authors: Hudson, Petera Whaiao

subjects: whakawhanaungatanga

abstract: Tertiary institutions in Aotearoa (New Zealand) offer students online teaching and learning papers across a variety of disciplines. The purpose of this research was to examine whether online teaching and learning environments in a tertiary institute provide opportunities to create conditions that promote te ao Māori (a Māori world view) aspirations for Māori scholars. Following a critical review of selected literature on how technologies and its pedagogical implications can realise cultural, educational, political and social aspirations in an online environment (see Chapter 2), the ethical practices according to Kaupapa Māori theory methodology, whakawhanaungatanga and spiral discourse is outlined (see Chapter 3). These practices together with spiral discourse and conversation analysis, were used to analyse the factors that facilitated or hindered optimal conditions that promoted teacher and student aspirations in the online environment (see Chapter 4). That analysis, conducted in relation to a number of focus points, revealed that when Māori practices of tikanga and ako pedagogy were applied in this realm, Māori scholars experienced the fulfilment of personal aspirations. Participants also experienced positive outcomes when whanaungatanga, the creation of interrelationships relationships between Māori students and teachers, whānau, friends, colleagues, was a focus together with good support facilities and services, and quality resources. This research supports the conclusion that online teaching and learning environments in a tertiary institute can provide opportunities to create conditions that promote te ao Māori aspirations for Māori scholars. Further investigations are needed to unravel the types and nature of the interrelationships between ako Māori pedagogies and the student and teacher, and whanaungatanga between students and other students that facilitate conditions that promoted Māori aspirations in an online environment.

text: Can te ao Māori worldviews exist within a western institute’s online teaching and learning environment? Tertiary institutions in Aotearoa (New Zealand) offer students online teaching and learning papers across a variety of disciplines. The purpose of this research was to examine whether online teaching and learning environments in a tertiary institute provide opportunities to create conditions that promote te ao Māori (a Māori world view) aspirations for Māori scholars. Following a critical review of selected literature on how technologies and its pedagogical implications can realise cultural, educational, political and social aspirations in an online environment (see Chapter 2), the ethical practices according to Kaupapa Māori theory methodology, whakawhanaungatanga and spiral discourse is outlined (see Chapter 3). These practices together with spiral discourse and conversation analysis, were used to analyse the factors that facilitated or hindered optimal conditions that promoted teacher and student aspirations in the online environment (see Chapter 4). That analysis, conducted in relation to a number of focus points, revealed that when Māori practices of tikanga and ako pedagogy were applied in this realm, Māori scholars experienced the fulfilment of personal aspirations. Participants also experienced positive outcomes when whanaungatanga, the creation of interrelationships relationships between Māori students and teachers, whānau, friends, colleagues, was a focus together with good support facilities and services, and quality resources. This research supports the conclusion that online teaching and learning environments in a tertiary institute can provide opportunities to create conditions that promote te ao Māori aspirations for Māori scholars. Further investigations are needed to unravel the types and nature of the interrelationships between ako Māori pedagogies and the student and teacher, and whanaungatanga between students and other students that facilitate conditions that promoted Māori aspirations in an online environment.

year: 2020