Andrew F Feldman
Biographic Data
| ID | 6823078 |
|---|---|
| NAME | Andrew F Feldman |
| GIVEN NAMES | Andrew F |
| FAMILY NAME | Feldman |
| SIGNATURE | FELDMAN A F |
| AFFILIATIONS | Goddard Space Flight Center |
| ORCID | 0000-0003-1547-6995 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2022 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 0 |
Responses of terrestrial ecosystem respiration to soil moisture across Australia
The terrestrial biosphere is the largest net sink of global CO 2 , but its sink capacity varies considerably from year to year depending on environmental conditions. Recent work has highlighted the importance of semi-arid ecosystems in interannually driving global concentrations of atmospheric CO 2 . We therefore need to better understand the dynamics and drivers of the CO 2 fluxes and their modeling along semi-arid to humid gradients. Respiratio…
Intraseasonal variability of vegetation water content in India driven by monsoon hydrometeorology
Understanding how Indian vegetation during the summer monsoon (June–September) responds to intraseasonal variability, with hydrometeorological stressors like vapor pressure deficit (VPD) and soil moisture (SM), is crucial and yet it is not well-explored. Existing studies often rely on correlation analysis and occasionally use causal inference, but they tend to overlook the intraseasonal scales of monsoon variability and their impact on vegetation…
Are rootzone soil moisture dynamics and thresholds associated with surface layer
The identification of evapotranspiration regimes, primarily the water-limited and energy-limited regimes, separated by the critical soil moisture (CSM) threshold, is fundamental to analyzing land–atmosphere interactions. To better understand the soil moisture (SM) dynamics happening synchronously in the soil column, we aim to estimate the rootzone (0–28 cm and 0–100 cm) CSM thresholds and associated regimes at a global scale, which was not previo…
Climate change-induced peatland drying in Southeast Asia
When organic peat soils are sufficiently dry, they become flammable. In Southeast Asian peatlands, widespread deforestation and associated drainage create dry conditions that, when coupled with El Niño-driven drought, result in catastrophic fire events that release large amounts of carbon and deadly smoke to the atmosphere. While the effects of anthropogenic degradation on peat moisture and fire risk have been extensively demonstrated, climate ch…
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Climate change-induced peatland drying in Southeast Asia
When organic peat soils are sufficiently dry, they become flammable. In Southeast Asian peatlands, widespread deforestation and associated drainage create dry conditions that, when coupled with El Niño-driven drought, result in catastrophic fire events that release large amounts of carbon and deadly smoke to the atmosphere. While the effects of anthropogenic degradation on peat moisture and fire risk have been extensively demonstrated, climate ch…
Are rootzone soil moisture dynamics and thresholds associated with surface layer
The identification of evapotranspiration regimes, primarily the water-limited and energy-limited regimes, separated by the critical soil moisture (CSM) threshold, is fundamental to analyzing land–atmosphere interactions. To better understand the soil moisture (SM) dynamics happening synchronously in the soil column, we aim to estimate the rootzone (0–28 cm and 0–100 cm) CSM thresholds and associated regimes at a global scale, which was not previo…
Responses of terrestrial ecosystem respiration to soil moisture across Australia
The terrestrial biosphere is the largest net sink of global CO 2 , but its sink capacity varies considerably from year to year depending on environmental conditions. Recent work has highlighted the importance of semi-arid ecosystems in interannually driving global concentrations of atmospheric CO 2 . We therefore need to better understand the dynamics and drivers of the CO 2 fluxes and their modeling along semi-arid to humid gradients. Respiratio…
Intraseasonal variability of vegetation water content in India driven by monsoon hydrometeorology
Understanding how Indian vegetation during the summer monsoon (June–September) responds to intraseasonal variability, with hydrometeorological stressors like vapor pressure deficit (VPD) and soil moisture (SM), is crucial and yet it is not well-explored. Existing studies often rely on correlation analysis and occasionally use causal inference, but they tend to overlook the intraseasonal scales of monsoon variability and their impact on vegetation…
Environmental Science (4 works) · Geography (4 works) · Geology (4 works) · Meteorology (4 works) · Moisture (3 works) · Soil Science (3 works) · Water content (3 works) · Climatology (2 works) · Ecology (2 works) · Hydrology (agriculture (2 works)