Jack Hutchings
Biographic Data
| ID | 6372161 |
|---|---|
| NAME | Jack Hutchings |
| GIVEN NAMES | Jack |
| FAMILY NAME | Hutchings |
| SIGNATURE | HUTCHINGS J |
| AFFILIATIONS | Washington University in St. Louis |
| ORCID | 0000-0003-3396-6787 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2018 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 0 |
Mid- to late-Holocene hydroclimate and vegetation changes near the Amazon-Tapajós confluence
The rainforests and freshwater resources of lowland Amazonia depend on precipitation from the Intertropical Convergence Zone (ITCZ) and the South American Summer Monsoon (SASM). However, our understanding of the climate and vegetation history of lowland Amazonia, particularly its response to the dynamics of the ITCZ and SASM, is limited by the lack of Holocene paleohydroclimate and paleoenvironmental records from eastern Amazonia. Here, we presen…
Divergent patterns of experimental and model-derived permafrost ecosystem carbon dynamics in response to Arctic warming
In the last few decades, temperatures in the Arctic have increased twice as much as the rest of the globe. As permafrost thaws in response to this warming, large amounts of soil organic matter may become vulnerable to decomposition. Microbial decomposition will release carbon (C) from permafrost soils, however, warmer conditions could also lead to enhanced plant growth and C uptake. Field and modeling studies show high uncertainty in soil and pla…
No prominent works on this page.
Divergent patterns of experimental and model-derived permafrost ecosystem carbon dynamics in response to Arctic warming
In the last few decades, temperatures in the Arctic have increased twice as much as the rest of the globe. As permafrost thaws in response to this warming, large amounts of soil organic matter may become vulnerable to decomposition. Microbial decomposition will release carbon (C) from permafrost soils, however, warmer conditions could also lead to enhanced plant growth and C uptake. Field and modeling studies show high uncertainty in soil and pla…
Mid- to late-Holocene hydroclimate and vegetation changes near the Amazon-Tapajós confluence
The rainforests and freshwater resources of lowland Amazonia depend on precipitation from the Intertropical Convergence Zone (ITCZ) and the South American Summer Monsoon (SASM). However, our understanding of the climate and vegetation history of lowland Amazonia, particularly its response to the dynamics of the ITCZ and SASM, is limited by the lack of Holocene paleohydroclimate and paleoenvironmental records from eastern Amazonia. Here, we presen…
Ecology (2 works) · Geology (2 works) · Amazon rainforest (1 work) · Amazonian Archaeology and Ethnohistory (1 work) · Archaeology (1 work) · Arctic (1 work) · Atmospheric sciences (1 work) · Carbon cycle (1 work) · Climate change (1 work) · Climate change and permafrost (1 work)