scholarly journals Migration Pathways for Frontline Care Workers in Australia and New Zealand: Front Doors, Side Doors, Back Doors and Trap Doors

2019 ◽  
Author(s):  
Joanna Howe ◽  
Sara Charlesworth ◽  
Deborah Brennan
Author(s):  
Joanna Howe ◽  
Sara Charlesworth ◽  
Deborah Brennan

This article examines the use of migration law and policy to address the labour needs of the care sector in two jurisdictions. New Zealand uses an Essential Skills visa to allow the direct entry of care workers on a temporary basis while Australia relies on a range of overseas born entrants including international students and working holiday makers, to meet labour supply challenges in the care sector and to supplement the local workforce, which includes many long-term permanent migrants. Changes to the work rights of working holiday makers, together with the introduction of a Designated Area Migration Agreement for Northern Australia and a Pacific Labour Scheme have created new opportunities for temporary entrants to work in care occupations but there is pressure on the Australian Government to open a dedicated temporary labour migration pathway for care workers. New Zealand’s revolving door of temporary migrant care workers and Australia’s de facto low skilled migration pathway both present regulatory challenges with regard to the protection of these workers in the labour market, their claims to citizenship and their opportunity to realise the ‘triple win’ promised in the temporary labour migration literature. The increasing reliance by Australia and New Zealand on temporary migrant care workers to meet the labour supply challenges in the sector also masks a range of other endemic employment relations problems in the sector (in particular, low pay) and may lead to a permanent demand for temporary migrant workers at the expense of local care workers.


2019 ◽  
Vol 2 ◽  
Author(s):  
Jed Montayre

New Zealand is an ethnically diverse nation. The number of overseas-born New Zealanders are increasing and migration pathways have added to the cultural diversity of New Zealand’s population. Acknowledging the health complexities experienced by older adults belonging to diverse cultural backgrounds is a growing research interest. This article aims to discuss the specific overlays between health and culture in the case of older Asian-New Zealanders by unpacking, presenting and critically analysing selected New Zealand studies. Based on this critical analysis, health-seeking behaviours and engagement with the healthcare system in New Zealand were influenced by cultural beliefs, traditional family values and the use of mainstream language. Understanding the overlaps between health and culture of the ageing ethnic groups is complex yet useful for health institutions. Furthermore, understanding the perspectives of ageing among ethnic and migrant groups within the context of cultural diversity is enhanced by considering an ethno-specific approach.  


2021 ◽  
Vol 12 ◽  
Author(s):  
Purushottama Bilimoria

We wake each morning to news on the glaring statistics of people infected by COVID-19 and others reportedly dying from complications thereto; the numbers are not receding in at least a number of countries across the world (barring a few that imposed strict lockdowns, testing and quarantining measures, such as Australia, Singapore, New Zealand and Vietnam). It is hard to imagine a moment such as this that most of us have lived through in our life-time; but it is a reality and public challenge that we can neither ignore nor look away from. In what follows I will explore perspectives on death from the Hindu tradition and the kinds of response—and solace or wisdom—afforded by the tradition to the angst and fears evoked by this pandemic situation. In concluding the discussion, I shall offer tentative reflections on how the Hindu perspective may be universalized, such as might invite conversations with therapists and care workers who may be seeking alternative resources to help expand the therapeutic space in more beneficent ways during the Covid-19 pandemic and its after-effects


2017 ◽  
Vol 26 (4) ◽  
pp. 480-504
Author(s):  
Oksana Opara

This article examines the Russian diaspora in New Zealand over the last 30 years. Using migration statistics and census data, post-communist migration trends and socio-economic outcomes of immigration from Russia to New Zealand are analyzed, to establish an empirical base for further qualitative and comparative investigation of the settlement experiences of Russian immigrants in New Zealand. Results reveal that the Russian diaspora has been growing, demonstrating spatial clustering in urban centers with the highest concentration in Auckland. While Russian immigrants have a high level of educational qualifications, their labor market outcomes have been weak and their income is lagging behind that of the New Zealand-born population and of migrants born in other countries. An over-representation of working-age female migrants is a distinctive feature of the Russian diaspora. Further research on the changing migration pathways and settlement strategies of the Russian immigrants in New Zealand is suggested.


2021 ◽  
Author(s):  
◽  
Hamish Cameron

<p>This study investigates the evolution (from initiation to inactivity) of a normal fault system in proximity to active petroleum systems within the Taranaki Basin, New Zealand. The aim of this research is to understand the evolution, interaction, and in some cases, death of normal faults in a region undergoing progressive regional extension. This research provides insight into the geometry, development, and displacement history of new and reactivated normal fault evolution through interpretation of industry standard seismic reflection data at high spatial and temporal resolution. Insight into normal fault evolution provides information on subsidence rates and potential hydrocarbon migration pathways.  Twelve time horizons between 1.2 and 35 Ma have been mapped throughout 1670 square kilometres of the Parihaka and Toro 3D seismic reflection surveys. Fault displacement analysis and backstripping have been used to determine the main phases of fault activity, fault growth patterns, and maximum Displacement/Length ratios. The timing, geometry, and displacement patterns for 110 normal faults with displacements >20 m have been interpreted and analysed using Paradigm SeisEarth and TrapTester 6 seismic interpretation and fault analysis software platforms.  Normal faults within the Parihaka and Toro 3D seismic surveys began developing at ˜11 Ma, with the largest faults accruing up to 1500 m of displacement in <10 Myr (mean throw displacement rate of 0.15mm/yr). Approximately 50% of the 110 mapped faults are associated with pre-existing normal faults and have typical cumulative displacements of ˜20 – 1000 m, with strike parallel lengths of <1 – 23 km. In contrast, new faults have typically greater displacements of 20 – 1400 m, and are generally longer with, with strike parallel lengths of ˜1 – 33 km.   New faults were the first faults within the system to become inactive when strain rates decreased from 0.06 – 0.03 between 3.6 and 3.0 Ma. Eight of the largest faults with > 1000 m cumulative displacement reach the seafloor and are potentially active at present day. An earthquake on one of these faults could be expected to produce MW 2.2 based on the maximum strike-parallel length of the fault plane.</p>


2014 ◽  
Vol 15 (3) ◽  
pp. 123-135 ◽  
Author(s):  
Celia Briar ◽  
Elizabeth Liddell ◽  
Martin Tolich

Purpose – The purpose of this paper is to focus on care workers employed in clients’ own homes recognising the skills and responsibilities of home-based care workers. Design/methodology/approach – Interviews and focus groups with domiciliary care workers in New Zealand centred on what these employees actually do during their working day. Findings – Home-based care workers require the same skills as residential care workers, but they also have greater responsibilities and receive less supervision and support, as they work largely in isolation. In addition, they must spend a large part of their working day travelling between clients: this time is unpaid, and brings their average hourly pay below the minimum wage. Practical implications – Although the home-based care workers who took part in this project love and are committed to making a positive difference to their clients, they also want the government, employers and the public to recognise their skills, efforts and their challenging working conditions. Originality/value – In earlier days of deinstitutionalisation, Graham described caring work as a “labour of love”. More than three decades years later, a New Zealand government minister described paid care workers as working partly “for love”. Care work is also currently perceived as unskilled. Both these perceptions depress the pay and working conditions of care staff, and in future may undermine the quality of care delivered to vulnerable clients.


2021 ◽  
Author(s):  
◽  
Hamish Cameron

<p>This study investigates the evolution (from initiation to inactivity) of a normal fault system in proximity to active petroleum systems within the Taranaki Basin, New Zealand. The aim of this research is to understand the evolution, interaction, and in some cases, death of normal faults in a region undergoing progressive regional extension. This research provides insight into the geometry, development, and displacement history of new and reactivated normal fault evolution through interpretation of industry standard seismic reflection data at high spatial and temporal resolution. Insight into normal fault evolution provides information on subsidence rates and potential hydrocarbon migration pathways.  Twelve time horizons between 1.2 and 35 Ma have been mapped throughout 1670 square kilometres of the Parihaka and Toro 3D seismic reflection surveys. Fault displacement analysis and backstripping have been used to determine the main phases of fault activity, fault growth patterns, and maximum Displacement/Length ratios. The timing, geometry, and displacement patterns for 110 normal faults with displacements >20 m have been interpreted and analysed using Paradigm SeisEarth and TrapTester 6 seismic interpretation and fault analysis software platforms.  Normal faults within the Parihaka and Toro 3D seismic surveys began developing at ˜11 Ma, with the largest faults accruing up to 1500 m of displacement in <10 Myr (mean throw displacement rate of 0.15mm/yr). Approximately 50% of the 110 mapped faults are associated with pre-existing normal faults and have typical cumulative displacements of ˜20 – 1000 m, with strike parallel lengths of <1 – 23 km. In contrast, new faults have typically greater displacements of 20 – 1400 m, and are generally longer with, with strike parallel lengths of ˜1 – 33 km.   New faults were the first faults within the system to become inactive when strain rates decreased from 0.06 – 0.03 between 3.6 and 3.0 Ma. Eight of the largest faults with > 1000 m cumulative displacement reach the seafloor and are potentially active at present day. An earthquake on one of these faults could be expected to produce MW 2.2 based on the maximum strike-parallel length of the fault plane.</p>


2021 ◽  
Author(s):  
◽  
Thomas Vasilios Golding

<p>Omakere Ridge is an anticlinal thrust ridge in water depths of 1100–1700mon the Hikurangi Margin, east of the North Island of New Zealand, and is an area of active seafloor methane seepage associated with an extensive gas hydrate province. Methane seep sites on the Hikurangi Margin are characterised by localised buildups of authigenic carbonate and chemosynthetic seep fauna that exist on a seafloor otherwise characterised by soft, muddy sediments and provide a unique window into the workings of the gas hydrate system. Seafloor methane seeps sites on Omakere Ridge have been successfully imaged using three newly-acquired acoustic datasets: a P-CableTM high-resolution 3D seismic reflection dataset (60 Hz); a multibeam sonar backscatter dataset (12 kHz); and a ParasoundTM subbottom profiler dataset (4 kHz). Seafloor seismic amplitude and similarity maps have been derived from a preliminary shipboard post-stack migrated data cube. A pronounced acquisition artifact is manifest in the seafloor horizon slice as high- and low-amplitude stripes that alternate periodically in the crossline direction. This artifact has been removed from the seafloor horizon slice using 2D spatial frequency filtering, followed by direct sampling and stochastic removal of the very-low-frequency components in the spatial domain. The seismic amplitude map has then been transformed into a calibrated seafloor reflection coefficient map. Sonar backscatter mosaics have been created after correcting for beam pattern effects and angular variation in backscatter after taking into account the bathymetry. Several backscatter mosaics were incorporated into a stacked mosaic over the study area to attenuate random noise. The ParasoundTM sub-bottom profiler data were processed to display instantaneous amplitude and separated into 43 lines over the study area. Comparison of 3D seismic attributes, multibeam backscatter intensity and shallow subsurface reflection characteristics provides new insights into the previously unknown extent of authigenic carbonate build-ups, methane migration pathways and seep initiation mechanisms at five seep sites on Omakere Ridge. Areas of high seafloor 3D seismic reflection coefficient and high multibeam backscatter intensity are interpreted as carbonate formations of at least 6–7 m thickness, while areas exhibiting low seismic reflection coefficient and moderate/high sonar backscatter intensity are interpreted as areas where the carbonates are less developed. Anomalous high-amplitude subsurface reflections beneath the seeps in the ParasoundTM data are interpreted as buried carbonates and may indicate a previously unknown earlier phase of seepage at Omakere Ridge, but could also be caused by gas or gas hydrates. The extent of authigenic carbonates is directly related to the duration of seepage and thus provides a new proxy for the chronology of seepage at Omakere Ridge, which has proved consistent with an existing hypothesis based on the abundance of deceased and live chemosynthetic fauna at the seep sites.</p>


2021 ◽  
Author(s):  
◽  
Thomas Vasilios Golding

<p>Omakere Ridge is an anticlinal thrust ridge in water depths of 1100–1700mon the Hikurangi Margin, east of the North Island of New Zealand, and is an area of active seafloor methane seepage associated with an extensive gas hydrate province. Methane seep sites on the Hikurangi Margin are characterised by localised buildups of authigenic carbonate and chemosynthetic seep fauna that exist on a seafloor otherwise characterised by soft, muddy sediments and provide a unique window into the workings of the gas hydrate system. Seafloor methane seeps sites on Omakere Ridge have been successfully imaged using three newly-acquired acoustic datasets: a P-CableTM high-resolution 3D seismic reflection dataset (60 Hz); a multibeam sonar backscatter dataset (12 kHz); and a ParasoundTM subbottom profiler dataset (4 kHz). Seafloor seismic amplitude and similarity maps have been derived from a preliminary shipboard post-stack migrated data cube. A pronounced acquisition artifact is manifest in the seafloor horizon slice as high- and low-amplitude stripes that alternate periodically in the crossline direction. This artifact has been removed from the seafloor horizon slice using 2D spatial frequency filtering, followed by direct sampling and stochastic removal of the very-low-frequency components in the spatial domain. The seismic amplitude map has then been transformed into a calibrated seafloor reflection coefficient map. Sonar backscatter mosaics have been created after correcting for beam pattern effects and angular variation in backscatter after taking into account the bathymetry. Several backscatter mosaics were incorporated into a stacked mosaic over the study area to attenuate random noise. The ParasoundTM sub-bottom profiler data were processed to display instantaneous amplitude and separated into 43 lines over the study area. Comparison of 3D seismic attributes, multibeam backscatter intensity and shallow subsurface reflection characteristics provides new insights into the previously unknown extent of authigenic carbonate build-ups, methane migration pathways and seep initiation mechanisms at five seep sites on Omakere Ridge. Areas of high seafloor 3D seismic reflection coefficient and high multibeam backscatter intensity are interpreted as carbonate formations of at least 6–7 m thickness, while areas exhibiting low seismic reflection coefficient and moderate/high sonar backscatter intensity are interpreted as areas where the carbonates are less developed. Anomalous high-amplitude subsurface reflections beneath the seeps in the ParasoundTM data are interpreted as buried carbonates and may indicate a previously unknown earlier phase of seepage at Omakere Ridge, but could also be caused by gas or gas hydrates. The extent of authigenic carbonates is directly related to the duration of seepage and thus provides a new proxy for the chronology of seepage at Omakere Ridge, which has proved consistent with an existing hypothesis based on the abundance of deceased and live chemosynthetic fauna at the seep sites.</p>


2005 ◽  
Vol 10 (2) ◽  
pp. 59-65 ◽  
Author(s):  
John Flynn ◽  
Elizabeth Foxon ◽  
Jim Lutz ◽  
Janine Pyrek

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