Aaron A Mohammed
Biographic Data
| ID | 7995586 |
|---|---|
| NAME | Aaron A Mohammed |
| GIVEN NAMES | Aaron A |
| FAMILY NAME | Mohammed |
| SIGNATURE | MOHAMMED A A |
| AFFILIATIONS | Dalhousie University |
| ORCID | 0000-0001-9037-1283 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 2 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2022 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 0 |
Mobilization of subsurface carbon pools driven by permafrost thaw and reactivation of groundwater flow: A virtual experiment
Permafrost thaw leads to an increase in groundwater circulation and potential mobilization of organic carbon sequestered in deep Arctic sediments (e.g. 3–25 m below surface). Upon thaw, a portion of this carbon may be transported along new groundwater flow paths to surface waters or be microbially transformed or immobilized by in-situ biogeochemical reactions. The fate of thaw-mobilized carbon impacts surface water productivity and global climate…
Sea-level rise and warming mediate coastal groundwater discharge in the Arctic
Groundwater discharge is an important mechanism through which fresh water and associated solutes are delivered to the ocean. Permafrost environments have traditionally been considered hydrogeologically inactive, yet with accelerated climate change and permafrost thaw, groundwater flow paths are activating and opening subsurface connections to the coastal zone. While warming has the potential to increase land-sea connectivity, sea-level change has…
No prominent works on this page.
Mobilization of subsurface carbon pools driven by permafrost thaw and reactivation of groundwater flow: A virtual experiment
Permafrost thaw leads to an increase in groundwater circulation and potential mobilization of organic carbon sequestered in deep Arctic sediments (e.g. 3–25 m below surface). Upon thaw, a portion of this carbon may be transported along new groundwater flow paths to surface waters or be microbially transformed or immobilized by in-situ biogeochemical reactions. The fate of thaw-mobilized carbon impacts surface water productivity and global climate…
Sea-level rise and warming mediate coastal groundwater discharge in the Arctic
Groundwater discharge is an important mechanism through which fresh water and associated solutes are delivered to the ocean. Permafrost environments have traditionally been considered hydrogeologically inactive, yet with accelerated climate change and permafrost thaw, groundwater flow paths are activating and opening subsurface connections to the coastal zone. While warming has the potential to increase land-sea connectivity, sea-level change has…
Aquifer (2 works) · Climate change and permafrost (2 works) · Cryospheric studies and observations (2 works) · Environmental Science (2 works) · Geology (2 works) · Groundwater (2 works) · Groundwater flow (2 works) · Hydrology (agriculture (2 works) · Oceanography (2 works) · Permafrost (2 works)