Intraoperative Monitoring of the Cochlear Nerve during Neurofibromatosis Type-2 Vestibular Schwannoma Surgery and Description of a "Test Intracochlear Electrode".

Objectives  A decision on whether to insert a cochlear implant can be made in neurofibromatosis 2 (NF2) if there is objective evidence of cochlear nerve (CN) function post vestibular schwannoma (VS) excision. We aimed to develop intraoperative CN monitoring to help in this decision. Design  We describe the intraoperative monitoring of a patient with NF2 and our stimulating and recording set up. A novel test electrode is used to stimulate the CN electrically. Setting  This study was set at a tertiary referral center for skull base pathology. Main outcome measure  Preserved auditory brainstem responses leading to cochlear implantation. Results  Electrical auditory brainstem response (EABR) waveforms will be displayed from different stages of the operation. A cochlear implant was inserted at the same sitting based on the EABR. Conclusion  Electrically evoked CN monitoring can provide objective evidence of CN function after VS excision and aid in the decision-making process of hearing rehabilitation in patients who will be rendered deaf

Low-Tech Riparian and Wet Meadow Restoration Increases Vegetation Productivity and Resilience Across Semiarid Rangelands

Restoration of riparian and wet meadow ecosystems in semiarid rangelands of the western United States is a high priority given their ecological and hydrological importance in the region. However, traditional restoration approaches are often intensive and costly, limiting the extent over which they can be applied. Practitioners are increasingly trying new restoration techniques that are more cost‐effective, less intensive, and can more practically scale up to the scope of degradation. Unfortunately, practitioners typically lack resources to undertake outcome‐based evaluations necessary to judge the efficacy of these techniques. In this study, we use freely available, satellite remote sensing to explore changes in vegetation productivity (normalized difference vegetation index) of three distinct, low‐tech, riparian and wet meadow restoration projects. Case studies are presented that range in geographic location (Colorado, Oregon, and Nevada), restoration practice (Zeedyk structures, beaver dam analogs, and grazing management), and time since implementation. Restoration practices resulted in increased vegetation productivity of up to 25% and increased annual persistence of productive vegetation. Improvements in productivity with time since restoration suggest that elevated resilience may further enhance wildlife habitat and increase forage production. Long‐term, documented outcomes of conservation are rare; we hope our findings empower practitioners to further monitor and explore the use of low‐tech methods for restoration of ecohydrologic processes at meaningful spatial scales

Climate Change: Scenarios & Impacts for Ireland (2000-LS-5.2.1-M1) ISBN:1-84095-115-X

The Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2001) is the most authoritative assessment of global climate change to date. Produced by several hundred leading scientists in various areas of climate studies, its principal conclusions include the following: • Global average temperature has increased by 0.6 ± 0.2°C since 1860 with accelerated warming apparent in the latter decades of the 20th century. A further increase of 1.5–6.0°C from 1990 to 2100 is projected, depending on how emissions of greenhouse gases increase over the period. • The 20th century was the warmest of the last millennium in the Northern Hemisphere, with the 1990s being the warmest decade and 1998 the warmest year. Warming has been more pronounced at night than during the day. • Reductions in the extent of snow cover of 10% have occurred in the past 40 years, with a widespread retreat also of mountain glaciers outside the polar regions. Sea-ice thickness in the Arctic has declined by about 40% during late summer/early autumn, though no comparable reduction has taken place in winter. In the Antarctic, no similar trends have been observed. One of the most serious impacts on global sea level could result from a catastrophic failure of grounded ice in West Antarctica. This is, however, considered unlikely over the coming century. • Global sea level has risen by 0.1–0.2 m over the past century, an order of magnitude larger than the average rate over the past three millennia. A rise of approximately 0.5 m is considered likely during the period 1990–2100. • Precipitation has increased over the land masses of the temperate regions by 0.5–1.0% per decade. Frequencies of more intense rainfall events appear to be increasing also in the Northern Hemisphere. In contrast, decreases in rainfall over the tropics have been observed, though this trend has weakened in recent years. More frequent warm-phase El Niño events are occurring in the Pacific Basin. Precipitation increases are projected, particularly for winter, for middle and high latitudes in the Northern Hemisphere and for Antarctica. • No significant trends in the tropical cyclone climatology have been detected. These global trends have implications for the future course of Ireland’s climate which it is judicious to anticipate. This report presents an assessment of the magnitude and likely impacts of climate change in Ireland over the course of the current century. It approaches this by establishing scenarios for future Irish climate based on global climate model projections for the middle and last quarter of the present century. These projections are then used to assess probable impacts in key sectors such as agriculture, forestry, water resources, the coastal and marine environments and on biodiversity. The purpose of the report is to firstly identify where vulnerability to climate change exists in Ireland and what adjustments are likely in the operation of environmental systems in response to such changes. In some sectors, e.g. agriculture, some new opportunities may arise. In other instances, e.g. water resource management, long-term planning strategies will be necessary to mitigate adverse impacts. Long lead times for adjustment characterise many sectors, e.g. forestry, and it is important to provide as much advance warning of likely changes as possible to enable adaptation to commence early. By anticipating change it may be possible to minimise adverse impacts and to maximise positive aspects of global climate change

Climate Change: Scenarios & Impacts for Ireland (2000-LS-5.2.1-M1) ISBN:1-84095-115-X

The Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2001) is the most authoritative assessment of global climate change to date. Produced by several hundred leading scientists in various areas of climate studies, its principal conclusions include the following: • Global average temperature has increased by 0.6 ± 0.2°C since 1860 with accelerated warming apparent in the latter decades of the 20th century. A further increase of 1.5–6.0°C from 1990 to 2100 is projected, depending on how emissions of greenhouse gases increase over the period. • The 20th century was the warmest of the last millennium in the Northern Hemisphere, with the 1990s being the warmest decade and 1998 the warmest year. Warming has been more pronounced at night than during the day. • Reductions in the extent of snow cover of 10% have occurred in the past 40 years, with a widespread retreat also of mountain glaciers outside the polar regions. Sea-ice thickness in the Arctic has declined by about 40% during late summer/early autumn, though no comparable reduction has taken place in winter. In the Antarctic, no similar trends have been observed. One of the most serious impacts on global sea level could result from a catastrophic failure of grounded ice in West Antarctica. This is, however, considered unlikely over the coming century. • Global sea level has risen by 0.1–0.2 m over the past century, an order of magnitude larger than the average rate over the past three millennia. A rise of approximately 0.5 m is considered likely during the period 1990–2100. • Precipitation has increased over the land masses of the temperate regions by 0.5–1.0% per decade. Frequencies of more intense rainfall events appear to be increasing also in the Northern Hemisphere. In contrast, decreases in rainfall over the tropics have been observed, though this trend has weakened in recent years. More frequent warm-phase El Niño events are occurring in the Pacific Basin. Precipitation increases are projected, particularly for winter, for middle and high latitudes in the Northern Hemisphere and for Antarctica. • No significant trends in the tropical cyclone climatology have been detected. These global trends have implications for the future course of Ireland’s climate which it is judicious to anticipate. This report presents an assessment of the magnitude and likely impacts of climate change in Ireland over the course of the current century. It approaches this by establishing scenarios for future Irish climate based on global climate model projections for the middle and last quarter of the present century. These projections are then used to assess probable impacts in key sectors such as agriculture, forestry, water resources, the coastal and marine environments and on biodiversity. The purpose of the report is to firstly identify where vulnerability to climate change exists in Ireland and what adjustments are likely in the operation of environmental systems in response to such changes. In some sectors, e.g. agriculture, some new opportunities may arise. In other instances, e.g. water resource management, long-term planning strategies will be necessary to mitigate adverse impacts. Long lead times for adjustment characterise many sectors, e.g. forestry, and it is important to provide as much advance warning of likely changes as possible to enable adaptation to commence early. By anticipating change it may be possible to minimise adverse impacts and to maximise positive aspects of global climate change

Climate Change: Scenarios & Impacts for Ireland (2000-LS-5.2.1-M1) ISBN:1-84095-115-X

The Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2001) is the most authoritative assessment of global climate change to date. Produced by several hundred leading scientists in various areas of climate studies, its principal conclusions include the following: • Global average temperature has increased by 0.6 ± 0.2°C since 1860 with accelerated warming apparent in the latter decades of the 20th century. A further increase of 1.5–6.0°C from 1990 to 2100 is projected, depending on how emissions of greenhouse gases increase over the period. • The 20th century was the warmest of the last millennium in the Northern Hemisphere, with the 1990s being the warmest decade and 1998 the warmest year. Warming has been more pronounced at night than during the day. • Reductions in the extent of snow cover of 10% have occurred in the past 40 years, with a widespread retreat also of mountain glaciers outside the polar regions. Sea-ice thickness in the Arctic has declined by about 40% during late summer/early autumn, though no comparable reduction has taken place in winter. In the Antarctic, no similar trends have been observed. One of the most serious impacts on global sea level could result from a catastrophic failure of grounded ice in West Antarctica. This is, however, considered unlikely over the coming century. • Global sea level has risen by 0.1–0.2 m over the past century, an order of magnitude larger than the average rate over the past three millennia. A rise of approximately 0.5 m is considered likely during the period 1990–2100. • Precipitation has increased over the land masses of the temperate regions by 0.5–1.0% per decade. Frequencies of more intense rainfall events appear to be increasing also in the Northern Hemisphere. In contrast, decreases in rainfall over the tropics have been observed, though this trend has weakened in recent years. More frequent warm-phase El Niño events are occurring in the Pacific Basin. Precipitation increases are projected, particularly for winter, for middle and high latitudes in the Northern Hemisphere and for Antarctica. • No significant trends in the tropical cyclone climatology have been detected. These global trends have implications for the future course of Ireland’s climate which it is judicious to anticipate. This report presents an assessment of the magnitude and likely impacts of climate change in Ireland over the course of the current century. It approaches this by establishing scenarios for future Irish climate based on global climate model projections for the middle and last quarter of the present century. These projections are then used to assess probable impacts in key sectors such as agriculture, forestry, water resources, the coastal and marine environments and on biodiversity. The purpose of the report is to firstly identify where vulnerability to climate change exists in Ireland and what adjustments are likely in the operation of environmental systems in response to such changes. In some sectors, e.g. agriculture, some new opportunities may arise. In other instances, e.g. water resource management, long-term planning strategies will be necessary to mitigate adverse impacts. Long lead times for adjustment characterise many sectors, e.g. forestry, and it is important to provide as much advance warning of likely changes as possible to enable adaptation to commence early. By anticipating change it may be possible to minimise adverse impacts and to maximise positive aspects of global climate change

Climate Change: Scenarios & Impacts for Ireland (2000-LS-5.2.1-M1) ISBN:1-84095-115-X

The Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2001) is the most authoritative assessment of global climate change to date. Produced by several hundred leading scientists in various areas of climate studies, its principal conclusions include the following: • Global average temperature has increased by 0.6 ± 0.2°C since 1860 with accelerated warming apparent in the latter decades of the 20th century. A further increase of 1.5–6.0°C from 1990 to 2100 is projected, depending on how emissions of greenhouse gases increase over the period. • The 20th century was the warmest of the last millennium in the Northern Hemisphere, with the 1990s being the warmest decade and 1998 the warmest year. Warming has been more pronounced at night than during the day. • Reductions in the extent of snow cover of 10% have occurred in the past 40 years, with a widespread retreat also of mountain glaciers outside the polar regions. Sea-ice thickness in the Arctic has declined by about 40% during late summer/early autumn, though no comparable reduction has taken place in winter. In the Antarctic, no similar trends have been observed. One of the most serious impacts on global sea level could result from a catastrophic failure of grounded ice in West Antarctica. This is, however, considered unlikely over the coming century. • Global sea level has risen by 0.1–0.2 m over the past century, an order of magnitude larger than the average rate over the past three millennia. A rise of approximately 0.5 m is considered likely during the period 1990–2100. • Precipitation has increased over the land masses of the temperate regions by 0.5–1.0% per decade. Frequencies of more intense rainfall events appear to be increasing also in the Northern Hemisphere. In contrast, decreases in rainfall over the tropics have been observed, though this trend has weakened in recent years. More frequent warm-phase El Niño events are occurring in the Pacific Basin. Precipitation increases are projected, particularly for winter, for middle and high latitudes in the Northern Hemisphere and for Antarctica. • No significant trends in the tropical cyclone climatology have been detected. These global trends have implications for the future course of Ireland’s climate which it is judicious to anticipate. This report presents an assessment of the magnitude and likely impacts of climate change in Ireland over the course of the current century. It approaches this by establishing scenarios for future Irish climate based on global climate model projections for the middle and last quarter of the present century. These projections are then used to assess probable impacts in key sectors such as agriculture, forestry, water resources, the coastal and marine environments and on biodiversity. The purpose of the report is to firstly identify where vulnerability to climate change exists in Ireland and what adjustments are likely in the operation of environmental systems in response to such changes. In some sectors, e.g. agriculture, some new opportunities may arise. In other instances, e.g. water resource management, long-term planning strategies will be necessary to mitigate adverse impacts. Long lead times for adjustment characterise many sectors, e.g. forestry, and it is important to provide as much advance warning of likely changes as possible to enable adaptation to commence early. By anticipating change it may be possible to minimise adverse impacts and to maximise positive aspects of global climate change

Climate Change: Scenarios & Impacts for Ireland (2000-LS-5.2.1-M1) ISBN:1-84095-115-X

The Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2001) is the most authoritative assessment of global climate change to date. Produced by several hundred leading scientists in various areas of climate studies, its principal conclusions include the following: • Global average temperature has increased by 0.6 ± 0.2°C since 1860 with accelerated warming apparent in the latter decades of the 20th century. A further increase of 1.5–6.0°C from 1990 to 2100 is projected, depending on how emissions of greenhouse gases increase over the period. • The 20th century was the warmest of the last millennium in the Northern Hemisphere, with the 1990s being the warmest decade and 1998 the warmest year. Warming has been more pronounced at night than during the day. • Reductions in the extent of snow cover of 10% have occurred in the past 40 years, with a widespread retreat also of mountain glaciers outside the polar regions. Sea-ice thickness in the Arctic has declined by about 40% during late summer/early autumn, though no comparable reduction has taken place in winter. In the Antarctic, no similar trends have been observed. One of the most serious impacts on global sea level could result from a catastrophic failure of grounded ice in West Antarctica. This is, however, considered unlikely over the coming century. • Global sea level has risen by 0.1–0.2 m over the past century, an order of magnitude larger than the average rate over the past three millennia. A rise of approximately 0.5 m is considered likely during the period 1990–2100. • Precipitation has increased over the land masses of the temperate regions by 0.5–1.0% per decade. Frequencies of more intense rainfall events appear to be increasing also in the Northern Hemisphere. In contrast, decreases in rainfall over the tropics have been observed, though this trend has weakened in recent years. More frequent warm-phase El Niño events are occurring in the Pacific Basin. Precipitation increases are projected, particularly for winter, for middle and high latitudes in the Northern Hemisphere and for Antarctica. • No significant trends in the tropical cyclone climatology have been detected. These global trends have implications for the future course of Ireland’s climate which it is judicious to anticipate. This report presents an assessment of the magnitude and likely impacts of climate change in Ireland over the course of the current century. It approaches this by establishing scenarios for future Irish climate based on global climate model projections for the middle and last quarter of the present century. These projections are then used to assess probable impacts in key sectors such as agriculture, forestry, water resources, the coastal and marine environments and on biodiversity. The purpose of the report is to firstly identify where vulnerability to climate change exists in Ireland and what adjustments are likely in the operation of environmental systems in response to such changes. In some sectors, e.g. agriculture, some new opportunities may arise. In other instances, e.g. water resource management, long-term planning strategies will be necessary to mitigate adverse impacts. Long lead times for adjustment characterise many sectors, e.g. forestry, and it is important to provide as much advance warning of likely changes as possible to enable adaptation to commence early. By anticipating change it may be possible to minimise adverse impacts and to maximise positive aspects of global climate change

The Vehicle, Fall 1985

Vol. 27, No. 1 Table of Contents Satchel AssMichael D. Smithpage 3 PhotoDoug Andersonpage 7 CounselingChristy Dunphypage 8 Grave SiteJay D. Fiskpage 8 Sight-Seeing Outside PhoenixBob Zordanipage 9 PerformanceDan Von Holtenpage 10 NightmareKandy Bellpage 10 Photo (The Loft)Lawrence McGownpage 11 LaboringJanet Gracepage 12 Blood DonorDan Von Holtenpage 13 Photo (Pier)Lawrence McGownpage 14 ExamplesChristopher Albinpage 14 Three PoemsPatrick Peterspage 15 Sometimes I Dream in Cotton CandyKathy Graypage 16 One Day While BoatingF. Link Rapierpage 17 DepartureBob Zordanipage 17 140 Print That\u27s Life Peter Dowlingpage 18 Photo (Around the Bend)Mike Freckerpage 20 Light ConversationDan Hintzpage 22 She Waits For the WorldJim Harrispage 22 HoneyKathy Graypage 23 Photo AlbumPatrick Peterspage 24 Photo (Stairs)Lawrence McGownpage 25 Fallen From Grace to SaturdayF. Link Rapierpage 26 Post MortemF. Link Rapierpage 27 ConfessionJohn Kayserpage 27 Child\u27s PlayChristopher Albinpage 27 Seeking A Friend\u27s Advice on DietingKathy Graypage 28 PhotoDoug Andersonpage 28 She Came Back to MeJim Harrispage 29 Farm BoyDiana Winsonpage 30 DilemmaJanet Wilhelmpage 31 In a Rock or StoneRichard Donnellypage 32 In November He Came To MeJean Kover Chandlerpage 33 EndingChristy Dunphypage 34 The Honor GradEddie Simpsonpage 35 Photo (Thirst)Mike Freckerpage 40https://thekeep.eiu.edu/vehicle/1046/thumbnail.jp

Evaluating the effectiveness and reliability of the Vibrant Soundbridge and Bonebridge auditory implants in clinical practice: Study design and methods for a multi-centre longitudinal observational study.

BACKGROUND: The Vibrant Soundbridge middle ear implant and the Bonebridge bone conducting hearing device are hearing implants that use radio frequency transmission to send information from the sound processor to the internal transducer. This reduces the risk of skin problems and infection but requires a more involved surgical procedure than competitor skin penetrating devices. It is not known whether more complex surgery will lead to additional complications. There is little information available on the reliability of these systems and adverse medical or surgical events. The primary research question is to determine the reliability and complication rate for the Vibrant Soundbridge and Bonebridge. The secondary research question explores changes in quality of life following implantation of the devices. The tertiary research question looks at effectiveness via changes in auditory performance. METHOD: The study was designed based on a combination of a literature search, two clinician focus groups and expert review.A multi-centre longitudinal observational study was designed. There are three study groups, two will have been implanted prior to the start of the study and one group, the prospective group, will be implanted after initiation of the study. Outcomes are surgical questionnaires, measures of quality of life, user satisfaction and speech perception tests in quiet and in noise. CONCLUSION: This is the first multi-centre study to look at these interventions and includes follow up over time to understand effectiveness, reliability, quality of life and complications

Preliminary Assessment of the Efficacy of a T-Cell–Based Influenza Vaccine, MVA-NP+M1, in Humans

A single vaccination with MVA-NP+M1 boosts T-cell responses to conserved influenza antigens in humans. Protection against influenza disease and virus shedding was demonstrated in an influenza virus challenge study