Evaluation of the potential impact of methane clathrate destabilization on future global warming

1995 ◽  
Vol 100 (D2) ◽  
pp. 2905 ◽  
Author(s):  
L. D. Danny Harvey ◽  
Zhen Huang
Keyword(s):  
Global Warming ◽  
Future Global Warming ◽  
Potential Impact ◽  
Methane Clathrate

Potential impact of global warming on deciduous oak dieback caused by ambrosia fungus Raffaelea sp. carried by ambrosia beetle Platypus quercivorus (Coleoptera: Platypodidae) in Japan

2002 ◽  
Vol 92 (2) ◽  
pp. 119-126 ◽  
Author(s):  
N. Kamata ◽  
K. Esaki ◽  
K. Kato ◽  
Y. Igeta ◽  
K. Wada
Keyword(s):  
Global Warming ◽  
Reproductive Success ◽  
Evolutionary Process ◽  
Ambrosia Beetle ◽  
Quercus Crispula ◽  
Platypus Quercivorus ◽  
Stable Relationship ◽  
Future Global Warming ◽  
Potential Impact ◽  
Associated Species

AbstractDeciduous oak dieback in Japan has been known since the 1930s, but in the last ten years epidemics have intensified and spread to the island’s western coastal areas. The symbiotic ambrosia fungus Raffaelea sp. is the causal agent of oak dieback, and is vectored by Platypus quercivorus (Murayama). This is the first example of an ambrosia beetle fungus that kills vigorous trees. Mortality of Quercus crispula was approximately 40% but much lower for associated species of Fagaceae, even though each species had a similar number of beetle attacks. It is likely that other oaks resistant to the fungus evolved under a stable relationship between the tree, fungus and beetle during a long evolutionary process. Quercus crispula was probably not part of this coevolution. This hypothesis was supported by the fact that P. quercivorus showed the least preference for Q. crispulayet exhibited highest reproductive success in this species. Therefore, P. quercivorus could spread more rapidly in stands with a high composition of Q. crispula. The present oak dieback epidemic in Japan probably resulted from the warmer climate that occurred from the late 1980s which made possible the fateful encounter of P. quercivorus with Q. cripsula by allowing the beetle to extend its distribution to more northerly latitudes and higher altitudes. Future global warming will possibly accelerate the overlapping of the distributions of P. quercivorus and Q. crispula with the result that oak dieback in Q. crispula will become more prevalent in Japan.

scholarly journals PLANT COMMUNITY CHANGE ACROSS THE PALEOCENE-EOCENE BOUNDARY IN THE GULF COASTAL PLAIN, CENTRAL TEXAS

2019 ◽  
Author(s):  
Jennifer D. Wagner ◽  
Daniel J. Peppe ◽  
Jennifer M.K. O'Keefe ◽  
Christopher Dennison
Keyword(s):  
Global Warming ◽  
Plant Community ◽  
Plant Communities ◽  
Coastal Plain ◽  
Community Change ◽  
Northern Great Plains ◽  
Gulf Coastal Plain ◽  
High Turnover ◽  
Future Global Warming ◽  
Central Texas

During the early Paleogene the Earth experienced long-term global warming punctuated by several short-term ‘hyperthermal’ events, the most pronounced of which is the Paleocene-Eocene Thermal Maximum (PETM). During this time, tropical climates expanded into extra-tropical areas potentially forming a wide band of ‘paratropical’ forests that are hypothesized to have expanded into the mid-latitude Northern Great Plains (NGP). Relatively little is known about these ‘paratropical’ floras, which would have extended across the Gulf Coastal Plain (GCP). This study assesses the preserved floras from the GCP in Central Texas before and after the PETM to define plant ecosystem changes associated with the hyperthermal event in this region. These floras suggest a high turnover rate, change in plant community composition, and uniform plant communities across the GCP at the Paleocene-Eocene boundary. Paleoecology and paleoclimate estimates from Central Texas PETM floras suggest a warm and wet environment, indicative of tropical seasonal forest to tropical rainforest biomes. Fossil evidence from the GCP combined with data from the NGP and modern tropics suggest that warming during the PETM helped create a ‘paratropical belt’ that extended into the mid-latitudes. Evaluating the response of plant communities to rapid global warming is important for understanding and preparing for current and future global warming and climate change.

scholarly journals Effective CO<sub>2</sub> lifetime and future CO<sub>2</sub> levels based on fit function

2013 ◽  
Vol 31 (9) ◽  
pp. 1591-1596 ◽  
Author(s):  
G. R. Sonnemann ◽  
M. Grygalashvyly
Keyword(s):  
Global Warming ◽  
Power Function ◽  
Co2 Emission ◽  
Emission Rates ◽  
Atmospheric Emissions ◽  
Atmospheric Concentration ◽  
Effective Lifetime ◽  
Global Emission ◽  
Future Global Warming ◽  
Atmospheric Co2 Concentrations

Abstract. The estimated global CO2 emission rates and the measured atmospheric CO2 concentrations show that only a certain share of the emitted CO2 accumulates in the atmosphere. For given atmospheric emissions of CO2, the effective lifetime determines its accumulation in the atmosphere and, consequently, its impact on the future global warming. We found that on average the inferred effective lifetime of CO2 decreases as its atmospheric concentration increases, reducing the rate of its accumulation in the atmosphere. We derived a power function that fits the varying lifetimes. Based on this fitting function, we calculated the increase of CO2 for different scenarios of future global emission rates.

Changing intensity and seasonality of wet extremes over Europe 

2021 ◽  
Author(s):  
Amal John ◽  
Hervé Douville ◽  
Pascal Yiou
Keyword(s):  
Global Warming ◽  
Daily Precipitation ◽  
Surface Air Temperature ◽  
Value Theory ◽  
Precipitation Extremes ◽  
Annual Maximum ◽  
Physical Mechanisms ◽  
Model Distribution ◽  
Future Global Warming ◽  
Global Mean

&lt;p&gt;Daily precipitation extremes are projected to intensify with global warming. Here the focus is on how extreme precipitation scales with the changing global mean surface air temperature (GSAT) and how much their inherent seasonality will change, using historical and SSP5-8.5 scenario simulations from 18 CMIP6 models for different sub-domains over Europe. With strong future global warming, the annual maximum precipitation (RX1DAY) is found to occur later in the year, although this shift is model-dependent and hardly significant in the multi-model distribution. Using generalized extreme value theory also provides evidence for the intensification of wet extremes in the future. In addition, we use monthly model outputs to decompose changes in RX1DAY occurring at the peak of the extreme season into several contributions, which gives insights into the underlying physical mechanisms that control the response of precipitation extremes and their inter-model spread.&lt;/p&gt;

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