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Comment on "Recent changes in climate extremes in the Caribbean region by Peterson et al. (2002)
(2009-10-26)
In a recent study, Peterson et al. (2002) analyzed daily temperature and rainfall data and concluded that “the climate of the Caribbean is changing” and that “these changes generally agreed with what is observed in many ...
Global warming projection of the change in dissolved oxygen concentrations in low oxygen regions of the oceans
(Universidad de Concepción.Facultad de Ciencias Naturales y Oceanográficas., 2006)
Deep time evidence for climate sensitivity increase with warming
(2016)
Future global warming from anthropogenic greenhouse gas emissions will depend on climate feedbacks, the effect of which is expressed by climate sensitivity, the warming for a doubling of atmospheric CO2 content. It is not ...
Climate change and tropical marine ecosystems: A review with an emphasis on coral reefs
(Universidad Estatal a Distancia de Costa Rica, 2019)
The intrinsic growth rate as a predictor of population viability under climate warming
(Wiley-Blackwell, 2013-11-01)
Lately, there has been interest in using the intrinsic growth rate (rm) to predict the effects of climate warming on ectotherm population viability. However, because rm is calculated using the Euler-Lotka equation, its ...
Design of non-motorized mobility plan for warm climate cities case: Hermosillo, Sonora, Mexico
(Agenda Ambiental, 2018)
Changes in climate at high southern latitudes: a unique daily record at Orcadas spanning 1903–2008
(American Meteorological Society, 2010-01)
The climate observations at Orcadas represent the only southern high-latitude site where data span more than a century, and its daily measurements are presented for the first time in this paper. Although limited to a single ...
Deep time evidence for climate sensitivity increase with warming
(Amer Geophysical Union, 2016)
Future global warming from anthropogenic greenhouse gas emissions will depend on climate feedbacks, the effect of which is expressed by climate sensitivity, the warming for a doubling of atmospheric CO2 content. It is not ...