Global projections of future wilderness decline under multiple IPCC Special Report on Emissions Scenarios

2022 ◽  
Vol 177 ◽  
pp. 105983
Author(s):  
Fangzheng Li ◽  
Wenyue Li ◽  
Fengyi Li ◽  
Ying Long ◽  
Shiyi Guo ◽  
...  
2003 ◽  
Vol 14 (2-3) ◽  
pp. 159-185 ◽  
Author(s):  
Ian Castles ◽  
David Henderson

This set of papers chiefly presents a critique of the IPCC's Special Report on Emissions Scenarios (SRES), which claims to “provide the basis for future assessments of climate change and possible response strategies”. The 40 scenarios are technically unsound in that, contrary to accepted international practice, they convert national GDP data to a common measure using market exchange rates. Because of this procedure and built-in assumptions about the extent to which the gap between rich and poor countries will be closed, the scenarios yield projections of GDP for developing regions which are improbably high: this includes the scenarios which give the lowest figures for projected cumulative emissions in the course of the century. Hence the SRES projections do not, as is claimed for them, encompass the full range of uncertainties about the future. Because of these and some other defects that we have noted, the SRES should not be taken as the accepted basis for the IPPC's coming Fourth Assessment Review. More broadly, the IPCC should try to ensure a more balanced, informed and professional treatment of the economic and statistical aspects of its work. In particular, there should be a greater involvement of economic ministries and statistical agencies.


2014 ◽  
Vol 27 (3) ◽  
pp. 1255-1270 ◽  
Author(s):  
Chad Shouquan Cheng ◽  
Edwina Lopes ◽  
Chao Fu ◽  
Zhiyong Huang

Abstract The methods used in earlier research focusing on the province of Ontario, Canada, were adapted for the current paper to expand the study area over the entire nation of Canada where various industries (e.g., transportation, agriculture, energy, and commerce) and infrastructure are at risk of being impacted by extreme wind gust events. The possible impacts of climate change on future wind gust events across Canada were assessed using a three-step process: 1) development and validation of hourly and daily wind gust simulation models, 2) statistical downscaling to derive future station-scale hourly wind speed data, and 3) projection of changes in the frequency of future wind gust events. The wind gust simulation models could capture the historically observed daily and hourly wind gust events. For example, the percentage of excellent and good validations for hourly wind gust events ≥90 km h−1 ranges from 62% to 85% across Canada; the corresponding percentage for wind gust events ≥40 km h−1 is about 90%. For future projection, the modeled results indicated that the frequencies of the wind gust events could increase late this century over Canada using the ensemble of the downscaled eight-GCM simulations [Special Report on Emissions Scenarios (SRES) A2 and B1]. For example, the percentage increases in future daily wind gust events ≥70 km h−1 from the current condition could be 10%–20% in most of the regions across Canada; the corresponding increases in future hourly wind gust events ≥70 km h−1 are projected to be 20%–30%. In addition, the inter-GCM and interscenario uncertainties of future wind gust projections were quantitatively assessed.


2005 ◽  
Vol 360 (1463) ◽  
pp. 2125-2138 ◽  
Author(s):  
Martin Parry ◽  
Cynthia Rosenzweig ◽  
Matthew Livermore

This paper reports the results of a series of research projects which have aimed to evaluate the implications of climate change for food production and risk of hunger. There are three sets of results: (a) for IS92a (previously described as a ‘business-as-usual’ climate scenario); (b) for stabilization scenarios at 550 and 750 ppm and (c) for Special Report on Emissions Scenarios (SRES). The main conclusions are: (i) the region of greatest risk is Africa; (ii) stabilization at 750 ppm avoids some but not most of the risk, while stabilization at 550 ppm avoids most of the risk and (iii) the impact of climate change on risk of hunger is influenced greatly by pathways of development. For example, a SRES B2 development pathway is characterized by much lower levels of risk than A2; and this is largely explained by differing levels of income and technology not by differing amounts of climate forcing.


2010 ◽  
Vol 23 (9) ◽  
pp. 2418-2427 ◽  
Author(s):  
Isaac M. Held ◽  
Michael Winton ◽  
Ken Takahashi ◽  
Thomas Delworth ◽  
Fanrong Zeng ◽  
...  

Abstract The fast and slow components of global warming in a comprehensive climate model are isolated by examining the response to an instantaneous return to preindustrial forcing. The response is characterized by an initial fast exponential decay with an e-folding time smaller than 5 yr, leaving behind a remnant that evolves more slowly. The slow component is estimated to be small at present, as measured by the global mean near-surface air temperature, and, in the model examined, grows to 0.4°C by 2100 in the A1B scenario from the Special Report on Emissions Scenarios (SRES), and then to 1.4°C by 2300 if one holds radiative forcing fixed after 2100. The dominance of the fast component at present is supported by examining the response to an instantaneous doubling of CO2 and by the excellent fit to the model’s ensemble mean twentieth-century evolution with a simple one-box model with no long times scales.


2003 ◽  
Vol 14 (4) ◽  
pp. 415-435 ◽  
Author(s):  
Ian Castles ◽  
David Henderson

This article restates and extends our critique of the economic and statistical work of the Intergovernmental Panel on Climate Change (IPCC), including in particular the Special Report on Emissions Scenarios (SRES). We respond to the article in the previous issue of Energy and Environment, in which 15 authors associated with the SRES argued against the case we had made there. We give reasons for rejecting their view that market exchange rates (MERs) should be used in deriving cross-country measures of economic growth, and note that in its handling of this and related issues they and others involved in the IPCC process are not professionally representative. We show how the mistaken use of MER-based comparisons, together with questionable assumptions about ‘closing the gap’ between rich countries and poor, have imparted an upward bias to projections of economic growth in developing countries, and hence to projections of total world emissions. We list actions that could be taken now, in the context of the IPCC's Fourth Assessment Review which is about to be launched, to set the economic and statistical aspects of the Review on a sounder basis. We argue that it is high time for ministries of economics and finance to inform themselves about the IPCC process and to become involved in it.


Biomédica ◽  
2017 ◽  
Vol 37 ◽  
pp. 106
Author(s):  
Jaime Badel-Mogollón ◽  
Laura Rodríguez-Figueroa ◽  
Gabriel Parra-Henao

Introducción. Ante el desconocimiento del contexto espacio-temporal de las condiciones biofísicas (hidrometereológicas y de densidad de la cobertura vegetal) de las zonas con presencia deTriatoma dimidiata en Santander y Boyacá, es necesario dilucidar los patrones asociados con estas variables para determinar su distribución y control.Objetivo. Hacer el análisis espacio-temporal de las variables biofísicas relacionadas con la distribución de Triatoma dimidiata de los departamentos de Santander y Boyacá en la región nororiental de Colombia.Materiales y métodos. Se utilizaron las bases de datos de los registros de presencia deT. dimidiata y de factores hidrometereológicos del Special Report on Emissions Scenarios (SRES) del Intergovernmental Panel on Climate Change, IPCC. Se estudiaron las variables de temperatura, humedad relativa, pluviosidad y densidad de la cobertura vegetal a nivel regional y local, se hizo el análisis espacial y el geoestadístico, así como el análisis estadístico descriptivo y temporal de las series de Fourier.Resultados. En las áreas con mayor presencia de T. dimidiata, las temperaturas a dos metros del suelo y en suelo cubierto oscilaron entre 14,5 y 18,8 °C, y la temperatura ambiente fue de 30 a 32 °C. La densidad de la cobertura vegetal y la pluviosidad en las áreas de mayor presencia de T. dimidiata exhibieron patrones de picos anuales y bienales. Los valores de la humedad relativa fluctuaron entre 66,8 y 85,1 %.Conclusiones. Las temperaturas a nivel de superficie y a dos metros del suelo fueron las variables determinantes de la distribución espacio-temporal de T. dimidiata. La elevada humedad relativa incentivó la búsqueda de refugios e incrementó la distribución geográfica en los picos anual y bienal de pluviosidad a nivel regional. Las condiciones ecológicas y antrópicas sugieren que T. dimidiata es una especie de gran resiliencia.


2004 ◽  
Vol 14 (2) ◽  
pp. 105-123 ◽  
Author(s):  
Stuart R. Gaffin ◽  
Cynthia Rosenzweig ◽  
Xiaoshi Xing ◽  
Greg Yetman

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