Jeremy W Lichstein
Biographic Data
| ID | 1573760 |
|---|---|
| NAME | Jeremy W Lichstein |
| GIVEN NAMES | Jeremy W |
| FAMILY NAME | Lichstein |
| SIGNATURE | LICHSTEIN J W |
| AFFILIATIONS | Princeton University |
| ORCID | 0000-0001-5553-6142 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2005 |
| LATEST PUBLICATION YEAR | 2021 |
| H-INDEX | 0 |
Surface water, vegetation, and fire as drivers of the terrestrial Arctic-boreal albedo feedback
The Arctic is warming twice as fast as the global average, due in part to the albedo feedbacks of a diminishing cryosphere. As snow cover extent decreases, the underlying land is exposed, which has lower albedo and therefore absorbs more radiation, warming the surface and causing a positive feedback to climate change. Changes in terrestrial snow-free albedo (e.g. changes in vegetation or surface water) could also affect Earth’s energy balance, bu…
Can Logging in Equatorial Africa Affect Adjacent Parks
Tropical deforestation can cause fundamental regional-scale shifts in vegetation structure and diversity. This is particularly true in Africa. Although national parks are being established to protect areas from deforestation and to conserve biodiversity, these parks are not immune to disturbances outside their boundaries. We used regional-scale atmospheric simulation experiments to investigate how deforestation in timber concessions might affect …
No prominent works on this page.
Can Logging in Equatorial Africa Affect Adjacent Parks
Tropical deforestation can cause fundamental regional-scale shifts in vegetation structure and diversity. This is particularly true in Africa. Although national parks are being established to protect areas from deforestation and to conserve biodiversity, these parks are not immune to disturbances outside their boundaries. We used regional-scale atmospheric simulation experiments to investigate how deforestation in timber concessions might affect …
Surface water, vegetation, and fire as drivers of the terrestrial Arctic-boreal albedo feedback
The Arctic is warming twice as fast as the global average, due in part to the albedo feedbacks of a diminishing cryosphere. As snow cover extent decreases, the underlying land is exposed, which has lower albedo and therefore absorbs more radiation, warming the surface and causing a positive feedback to climate change. Changes in terrestrial snow-free albedo (e.g. changes in vegetation or surface water) could also affect Earth’s energy balance, bu…
Environmental Science (2 works) · Geography (2 works) · Agroforestry (1 work) · Albedo (alchemy (1 work) · Antarctic sea ice (1 work) · Arctic (1 work) · Atmospheric sciences (1 work) · Boreal (1 work) · Climate change (1 work) · Climate change and permafrost (1 work)