Tootfinder

Climate benefits of afforestation and reforestation with varying species mixtures and densities in the north-western boreal lands
Enoch Ofosua, Kevin Bradley Dsouzaa, Daniel Chukwuemeka Amaogud, Jerome Pigeond, Richard Boudreaultc, Juan Moreno-Crubb, Pooneh Maghoule, Yuri Leonenko
https://arxiv.org/abs/2506.03300

Climate benefits of afforestation and reforestation with varying species mixtures and densities in the north-western boreal lands
The boreal forest plays a crucial role as a global carbon sink. This study uses two 250-year simulations of Canada's Taiga Plains, an area targeted by the 2 Billion Trees Program to evaluate afforestation and reforestation strategies that vary by species mix, planting density, and surface albedo. Medium density stands, 600 to 1400 trees per hectare, composed of mixed species with approximately 25 to 40 percent deciduous trees sequestered 15 to 30 percent more net ecosystem carbon than conifer m…

This https://arxiv.org/abs/2401.14230 has been replaced.
initial toot: https://mastoxiv.page/@arXi…

Unravelling how winds and surface heat fluxes control the Atlantic Oceans meridional heat transport
The North Atlantic Ocean circulation, fuelled by winds and surface buoyancy fluxes, carries 1.25 PettaWatts of heat poleward in the subtropics, and helps in regulating global weather and climate patterns. Here, we assess the relative impacts of changes in winds and surface heat fluxes on the Atlantic Ocean circulation and heat transport on short timescales (<10 years) and long timescales (>50 years) using ocean simulations. We decompose the circulation and heat transport into warm and cold cell…

This https://arxiv.org/abs/2401.14230 has been replaced.
initial toot: https://mastoxiv.page/@arXi…

Unravelling how winds and surface heat fluxes control the Atlantic Oceans meridional heat transport
The North Atlantic Ocean circulation, fuelled by winds and surface buoyancy fluxes, carries 1.25 PettaWatts of heat poleward in the subtropics, and helps in regulating global weather and climate patterns. Here, we assess the relative impacts of changes in winds and surface heat fluxes on the Atlantic Ocean circulation and heat transport on short timescales (<10 years) and long timescales (>50 years) using ocean simulations. We decompose the circulation and heat transport into warm and cold cell…