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What is MOCA? 

The MOCA project will enhance understanding of the present atmospheric effects of methane released from dissociation of gas hydrates in Arctic seabed sediments, and will also inform on the future potential impacts in a warming climate on decadal to centennial timescales. 

Methane hydrates (MH) in ocean seabed sediments are a potential source of methane (CH4) to the atmosphere, where CH4 has potential to act as a powerful greenhouse gas. Recent scientific results studies show diversity in the flux of CH4 that actually reaches the atmosphere. MH are potentially susceptible to ocean warming, which could trigger a positive feedback resulting in rapid climate warming. 

MOCA is funded by the Norwegian Research Council and will apply advanced measurements and modelling to quantify the amount and present atmospheric impact of CH4 originating from MH. Furthermore, the project will investigate potential future climate effects from destabilisation of MH deposits in a warming climate, and will focus on scenarios in 2050 and 2100. 



Summer cruise in the Barent's Sea


The summer 2015 Barent’s Sea cruise ended mid-July. In addition to the successful collection of online data on CH4, CO2, CO and flask samples for quantification of light hydrocarbons, two samples of pure gas hydrates have been taken from drill cores south of Svalbard earlier this summer. Quantification of the light hydrocarbons in these samples will give a clearer picture of how a hydrate signal would look if hydrate gases reach atmosphere.

 

   

 Anna Silyakova, CAGE, working with the methane samples, and transferring them to the new sampling equipment developed during MOCA for analysis at NILU.


  
 

         
                                                                                            
 
 Content related queries:  Cathrine Lund Myhre (clm 'at' nilu.no)