Randolph Kinney
Elite Member
- Joined
- Apr 7, 2005
- Professional Status
- Retired Appraiser
- State
- North Carolina
Methane Hydrates and Contemporary Climate Change
By: Carolyn D. Ruppel (U.S. Geological Survey, Woods Hole, MA) © 2011 Nature Education
Citation: Ruppel, C. D. (2011) Methane Hydrates and Contemporary Climate Change. Nature Education Knowledge 3(10):29
As the evidence for warming climate became better established in the latter part of the 20th century (IPCC 2001), some scientists raised the alarm that large quantities of methane (CH4) might be liberated by widespread destabilization of climate-sensitive gas hydrate deposits trapped in marine and permafrost-associated sediments (Bohannon 2008, Krey et al. 2009, Mascarelli 2009). Even if only a fraction of the liberated CH4 were to reach the atmosphere, the potency of CH4 as a greenhouse gas (GHG) and the persistence of its oxidative product (CO2) heightened concerns that gas hydrate dissociation could represent a slow tipping point (Archer et al. 2009) for Earth's contemporary period of climate change.
Methane Hydrate Primer
Methane hydrate is an ice-like substance formed when CH4 and water combine at low temperature (up to ~25ºC) and moderate pressure (greater than 3-5 MPa, which corresponds to combined water and sediment depths of 300 to 500 m). Globally, an estimated 99% of gas hydrates occurs in the sediments of marine continental margins at saturations as high as 20% to 80% in some lithologies; the remaining 1% is mostly associated with sediments in and beneath areas of high-latitude, continuous permafrost (McIver 1981, Collett et al. 2009). Nominally, methane hydrate concentrates CH4 by ~164 times on a volumetric basis compared to gas at standard pressure and temperature. Warming a small volume of gas hydrate could thus liberate large volumes of gas.
A challenge for assessing the impact of contemporary climate change on methane hydrates is continued uncertainty about the size of the global gas hydrate inventory and the portion of the inventory that is susceptible to climate warming. This paper addresses the latter issue, while the former remains under active debate. Dickens (2011) recently estimated 7x102 to 1.27x104 Gt carbon (Gt C) to be sequestered in marine gas hydrates alone, while Shakhova et al. (2010a) estimate 3.75x102 Gt C in methane hydrates just on the East Siberian Arctic shelf (ESAS). A conservative estimate (Boswell & Collett 2011) for the global gas hydrate inventory is ~1.8x103 Gt C, corresponding to CH4 volume of ~3.0x1015 m3 if CH4 density is taken as 0.717 kg/m3. In the unlikely event that 0.1% (1.8 Gt C) of this CH4 were instantaneously released to the atmosphere, CH4 concentrations would increase to ~2900 ppb from the 2005 value of ~1774 ppb (IPCC 2007).
http://www.nature.com/scitable/know...ates-and-contemporary-climate-change-24314790
Notice that the release of methane follows the rise of temperature. Is that strange? No and neither is the release of CO2 with rising temperatures.
The earth has been warming since the mini ice age of the 1600s. http://www.telegraph.co.uk/news/science/11733369/Earth-heading-for-mini-ice-age-within-15-years.html
By: Carolyn D. Ruppel (U.S. Geological Survey, Woods Hole, MA) © 2011 Nature Education
Citation: Ruppel, C. D. (2011) Methane Hydrates and Contemporary Climate Change. Nature Education Knowledge 3(10):29
As the evidence for warming climate became better established in the latter part of the 20th century (IPCC 2001), some scientists raised the alarm that large quantities of methane (CH4) might be liberated by widespread destabilization of climate-sensitive gas hydrate deposits trapped in marine and permafrost-associated sediments (Bohannon 2008, Krey et al. 2009, Mascarelli 2009). Even if only a fraction of the liberated CH4 were to reach the atmosphere, the potency of CH4 as a greenhouse gas (GHG) and the persistence of its oxidative product (CO2) heightened concerns that gas hydrate dissociation could represent a slow tipping point (Archer et al. 2009) for Earth's contemporary period of climate change.
Methane Hydrate Primer
Methane hydrate is an ice-like substance formed when CH4 and water combine at low temperature (up to ~25ºC) and moderate pressure (greater than 3-5 MPa, which corresponds to combined water and sediment depths of 300 to 500 m). Globally, an estimated 99% of gas hydrates occurs in the sediments of marine continental margins at saturations as high as 20% to 80% in some lithologies; the remaining 1% is mostly associated with sediments in and beneath areas of high-latitude, continuous permafrost (McIver 1981, Collett et al. 2009). Nominally, methane hydrate concentrates CH4 by ~164 times on a volumetric basis compared to gas at standard pressure and temperature. Warming a small volume of gas hydrate could thus liberate large volumes of gas.
A challenge for assessing the impact of contemporary climate change on methane hydrates is continued uncertainty about the size of the global gas hydrate inventory and the portion of the inventory that is susceptible to climate warming. This paper addresses the latter issue, while the former remains under active debate. Dickens (2011) recently estimated 7x102 to 1.27x104 Gt carbon (Gt C) to be sequestered in marine gas hydrates alone, while Shakhova et al. (2010a) estimate 3.75x102 Gt C in methane hydrates just on the East Siberian Arctic shelf (ESAS). A conservative estimate (Boswell & Collett 2011) for the global gas hydrate inventory is ~1.8x103 Gt C, corresponding to CH4 volume of ~3.0x1015 m3 if CH4 density is taken as 0.717 kg/m3. In the unlikely event that 0.1% (1.8 Gt C) of this CH4 were instantaneously released to the atmosphere, CH4 concentrations would increase to ~2900 ppb from the 2005 value of ~1774 ppb (IPCC 2007).
http://www.nature.com/scitable/know...ates-and-contemporary-climate-change-24314790
Notice that the release of methane follows the rise of temperature. Is that strange? No and neither is the release of CO2 with rising temperatures.
The earth has been warming since the mini ice age of the 1600s. http://www.telegraph.co.uk/news/science/11733369/Earth-heading-for-mini-ice-age-within-15-years.html
