Nest temperatures of the Piai and Sayang Islands green turtle
... estimated from the model of embryonic growth to determine the TSP duration. Hatchling sex ratio was estimated by the mean temperature, weighted by embryonic growth, during the middle third of development for each nest. The mean nest temperature during the middle third in each nest was compared to av ...
... estimated from the model of embryonic growth to determine the TSP duration. Hatchling sex ratio was estimated by the mean temperature, weighted by embryonic growth, during the middle third of development for each nest. The mean nest temperature during the middle third in each nest was compared to av ...
climate change and emissions pathways
... reasons for concern about climate change (ref. 3 and Fig. 1). Each category represents a semiindependent ‘‘consensus estimate’’ of a metric for measuring ‘‘concern’’ about the climate system. We view these metrics as indicators of the level of global mean temperature change associated with DAI in th ...
... reasons for concern about climate change (ref. 3 and Fig. 1). Each category represents a semiindependent ‘‘consensus estimate’’ of a metric for measuring ‘‘concern’’ about the climate system. We view these metrics as indicators of the level of global mean temperature change associated with DAI in th ...
Ozone hole and Southern Hemisphere climate change
... been increasing (decreasing) in the recent past [Son et al., 2009]. This trend is well captured by models with prescribed ozone depletion (red), but severely underestimated in its absence (green). The multimodel mean further suggests that, accompanying ozone recovery, tropopause height trends might ...
... been increasing (decreasing) in the recent past [Son et al., 2009]. This trend is well captured by models with prescribed ozone depletion (red), but severely underestimated in its absence (green). The multimodel mean further suggests that, accompanying ozone recovery, tropopause height trends might ...
Nullifying the climate null hypothesis
... and identifiable in the instrumental records of the last century-and-a-half and in recent paleoclimate records? The answer to this question depends on the null hypothesis against which such an impact is tested. The current approach that is generally pursued assumes essentially that past climate vari ...
... and identifiable in the instrumental records of the last century-and-a-half and in recent paleoclimate records? The answer to this question depends on the null hypothesis against which such an impact is tested. The current approach that is generally pursued assumes essentially that past climate vari ...
Diapositiva 1
... • More sensitivity to the users’ needs: going beyond downscaling, better documentation (e.g. use the IPCC language), demonstration of value and outreach. CMUG Integration Meeting – Satellite data sets for climate prediction and services ...
... • More sensitivity to the users’ needs: going beyond downscaling, better documentation (e.g. use the IPCC language), demonstration of value and outreach. CMUG Integration Meeting – Satellite data sets for climate prediction and services ...
Glacier variations and climate change in the central Himalaya over
... Thompson and others (2000) found that over relatively long timescales (decades to century) the trend in d18O from the Dasuopu ice core is similar to that of the Northern Hemisphere temperature history. This leads them to suggest that the d18O profiles from Himalayan ice cores might reflect long-term ...
... Thompson and others (2000) found that over relatively long timescales (decades to century) the trend in d18O from the Dasuopu ice core is similar to that of the Northern Hemisphere temperature history. This leads them to suggest that the d18O profiles from Himalayan ice cores might reflect long-term ...
Climate change in Australia | Central Slopes cluster report
... periods: the near future 2020–2039 (herein referred to as 2030) and late in the century 2080–2099 (herein referred to as 2090). The spread of model results are presented as the range between the 10th and 90th percentile in the CMIP5 ensemble output. For each time period, the model spread can be attr ...
... periods: the near future 2020–2039 (herein referred to as 2030) and late in the century 2080–2099 (herein referred to as 2090). The spread of model results are presented as the range between the 10th and 90th percentile in the CMIP5 ensemble output. For each time period, the model spread can be attr ...
Climate Change Strategy - Environment Yukon
... In Yukon, and across the circumpolar north, the effects of climate change are becoming more apparent and better understood. Yukon is experiencing impacts such as thawing permafrost, increased glacial melting, rising sea levels on the north coast, beetle infestations across southern spruce forests an ...
... In Yukon, and across the circumpolar north, the effects of climate change are becoming more apparent and better understood. Yukon is experiencing impacts such as thawing permafrost, increased glacial melting, rising sea levels on the north coast, beetle infestations across southern spruce forests an ...
Yukon Government Climate Change Strategy
... In Yukon, and across the circumpolar north, the effects of climate change are becoming more apparent and better understood. Yukon is experiencing impacts such as thawing permafrost, increased glacial melting, rising sea levels on the north coast, beetle infestations across southern spruce forests an ...
... In Yukon, and across the circumpolar north, the effects of climate change are becoming more apparent and better understood. Yukon is experiencing impacts such as thawing permafrost, increased glacial melting, rising sea levels on the north coast, beetle infestations across southern spruce forests an ...
The Role of Stochastic Forcing on the Behavior of Thermohaline
... a cooling with a maximum of 10 K over the nordic seas, while the spatial extent of the cooling is model dependent.8 In the last decade some efforts have been made to measure the magnitude of this circulation and even to determine if there is a diminishing trend in the actual context of climate chang ...
... a cooling with a maximum of 10 K over the nordic seas, while the spatial extent of the cooling is model dependent.8 In the last decade some efforts have been made to measure the magnitude of this circulation and even to determine if there is a diminishing trend in the actual context of climate chang ...
a discussion based on contributions from climate modeling
... In addition to the recovery of the past temperature evolution BTPs have also been used to evaluate the role of heat storage in the lithospheric crust within the global energy balance (Levitus et al., 2001; Pielke, 2003; Levitus et al., 2005; Hansen et al., 2005) by calculating the amount of energy s ...
... In addition to the recovery of the past temperature evolution BTPs have also been used to evaluate the role of heat storage in the lithospheric crust within the global energy balance (Levitus et al., 2001; Pielke, 2003; Levitus et al., 2005; Hansen et al., 2005) by calculating the amount of energy s ...
Climate change in the oceans: evolutionary
... which mostly deals with ocean warming, ocean acidification and deoxygenation. Marked warming trends in surface waters are apparent already today sometimes markedly exceeding atmospheric warming (Perry et al. 2005). Even water layers that are relatively isolated from the well-mixed surface ocean alre ...
... which mostly deals with ocean warming, ocean acidification and deoxygenation. Marked warming trends in surface waters are apparent already today sometimes markedly exceeding atmospheric warming (Perry et al. 2005). Even water layers that are relatively isolated from the well-mixed surface ocean alre ...
CLIMATE CHANGE IMPACTS IN NEW ZEALAND: A CROSS
... The key changes in Step 1 above were the climate projections from NIWA, demographics, social variables, and wildcard variables. In summary, for the social scenarios we assumed an overall growth in the New Zealand population up to over five million people by the 2080s with larger Maori, Pacific Islan ...
... The key changes in Step 1 above were the climate projections from NIWA, demographics, social variables, and wildcard variables. In summary, for the social scenarios we assumed an overall growth in the New Zealand population up to over five million people by the 2080s with larger Maori, Pacific Islan ...
The global distribution of cultivable lands: current
... revisit this problem. With the use of remotely sensed data, consistent, globally gridded land cover classification datasets have been developed to provide an accurate picture of current cropland distributions. Furthermore, new global datasets of soil properties have emerged in recent years. In this ...
... revisit this problem. With the use of remotely sensed data, consistent, globally gridded land cover classification datasets have been developed to provide an accurate picture of current cropland distributions. Furthermore, new global datasets of soil properties have emerged in recent years. In this ...
the whole inaugural address as pdf
... an integrity problem. The question raised is that of whether climate scientists are too much in alignment with policymakers when they pretend that climate change could still be limited to a global temperature increase of 2oC. Are all sorts of ‘dubious concepts’, such as negative emissions, now being ...
... an integrity problem. The question raised is that of whether climate scientists are too much in alignment with policymakers when they pretend that climate change could still be limited to a global temperature increase of 2oC. Are all sorts of ‘dubious concepts’, such as negative emissions, now being ...
Impacts of climate change on European marine ecosystems
... issue; Wernberg et al., 2011-this issue; all this volume). During the last 10–15 years, sea water temperatures throughout much of the globe have changed at unprecedented rates: sea ice cover in the Arctic is rapidly disappearing; melting of glaciers and the Greenland ice cap is accelerating; the vol ...
... issue; Wernberg et al., 2011-this issue; all this volume). During the last 10–15 years, sea water temperatures throughout much of the globe have changed at unprecedented rates: sea ice cover in the Arctic is rapidly disappearing; melting of glaciers and the Greenland ice cap is accelerating; the vol ...
NVCA Climate Change Strategy and Action Plan Milestone 1
... Setting the Stage – Initial Climate Change Research Climate Change in the Context of the Nottawasaga Valley In conjunction with the increasing concentration of greenhouse gases, it is certain that temperatures globally have been rising since the late 19th century and even more notably since the lat ...
... Setting the Stage – Initial Climate Change Research Climate Change in the Context of the Nottawasaga Valley In conjunction with the increasing concentration of greenhouse gases, it is certain that temperatures globally have been rising since the late 19th century and even more notably since the lat ...
Global response of terrestrial ecosystem structure and function to
... the terrestrial carbon sink, as far as it is generated by increasing CO2, still has the potential to increase but cannot persist inde®nitely at high strength (King et al. 1997; Cao & Woodward 1998). The eventual decline shown in these simulations has two main causes: on the one hand, the direct phys ...
... the terrestrial carbon sink, as far as it is generated by increasing CO2, still has the potential to increase but cannot persist inde®nitely at high strength (King et al. 1997; Cao & Woodward 1998). The eventual decline shown in these simulations has two main causes: on the one hand, the direct phys ...
Global warming hiatus
A global warming hiatus, also sometimes referred to as a global warming pause or a global warming slowdown, is a period of relatively little change in globally averaged surface temperatures. In the current episode of global warming many such periods are evident in the surface temperature record, along with robust evidence of the long term warming trend.The exceptionally warm El Niño year of 1998 was an outlier from the continuing temperature trend, and so gave the appearance of a hiatus: by January 2006 assertions had been made that this showed that global warming had stopped. A 2009 study showed that decades without warming were not exceptional, and in 2011 a study showed that if allowances were made for known variability, the rising temperature trend continued unabated. There was increased public interest in 2013 in the run-up to publication of the IPCC Fifth Assessment Report, and despite concerns that a 15-year period was too short to determine a meaningful trend, the IPCC included a section on a hiatus, which it defined as a much smaller increasing linear trend over the 15 years from 1998 to 2012, than over the 60 years from 1951 to 2012. Various studies examined possible causes of the short term slowdown. Even though the overall climate system had continued to accumulate energy due to Earth's positive energy budget, the available temperature readings at the earth's surface indicated slower rates of increase in surface warming than in the prior decade. Since measurements at the top of the atmosphere show that Earth is receiving more energy than it is radiating back into space, the retained energy should be producing warming in at least one of the five parts of Earth's climate system.A July 2015 paper on the updated NOAA dataset cast doubt on the existence of this supposed hiatus, and found no indication of a slowdown. This analysis incorporated the latest corrections for known biases in ocean temperature measurements, and new land temperature data. Scientists working on other datasets welcomed this study, though the view was expressed that the short term warming trend had been slower than in previous periods of the same length.