Maxwell Kelley
Biographic Data
| ID | 7997626 |
|---|---|
| NAME | Maxwell Kelley |
| GIVEN NAMES | Maxwell |
| FAMILY NAME | Kelley |
| SIGNATURE | KELLEY M |
| AFFILIATIONS | Goddard Institute for Space Studies |
| VERIFIED | No |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 1998 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 0 |
Responses of compound daytime and nighttime warm-dry and warm-humid events to individual anthropogenic forcings
Daytime heat is often associated with reduced soil moisture and cloud cover, while nighttime heat is connected to high humidity and increased cloud cover. Due to these differing mechanisms, compound daytime and nighttime heat events may respond differently to major anthropogenic forcings (greenhouse gases, anthropogenic aerosols, land-use and land-cover change). Here, we use GISS ModelE2.1-G historical single-forcing runs from 1955 to 2014 to exa…
A Reassessment of U-Th and 14 C Ages for Late-Glacial High-Frequency Hydrological Events at Searles Lake, California
U-Th isochron ages of tufas formed on shorelines suggest that the last pluvial event in Lake Lahontan and Searles Lake was synchronous at about 16,500 cal yr B.P. (equivalent to a radiocarbon age of between 14,000 and 13,500 yr B.P.), whereas the timing of this pluvial event determined by radiocarbon dating is on the order of 1000 yr younger. The timing of seven distinct periods of near desiccation in Searles Lake during late-glacial time has bee…
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A Reassessment of U-Th and 14 C Ages for Late-Glacial High-Frequency Hydrological Events at Searles Lake, California
U-Th isochron ages of tufas formed on shorelines suggest that the last pluvial event in Lake Lahontan and Searles Lake was synchronous at about 16,500 cal yr B.P. (equivalent to a radiocarbon age of between 14,000 and 13,500 yr B.P.), whereas the timing of this pluvial event determined by radiocarbon dating is on the order of 1000 yr younger. The timing of seven distinct periods of near desiccation in Searles Lake during late-glacial time has bee…
Responses of compound daytime and nighttime warm-dry and warm-humid events to individual anthropogenic forcings
Daytime heat is often associated with reduced soil moisture and cloud cover, while nighttime heat is connected to high humidity and increased cloud cover. Due to these differing mechanisms, compound daytime and nighttime heat events may respond differently to major anthropogenic forcings (greenhouse gases, anthropogenic aerosols, land-use and land-cover change). Here, we use GISS ModelE2.1-G historical single-forcing runs from 1955 to 2014 to exa…
Aerosol (1 work) · Atmospheric and Environmental Gas Dynamics (1 work) · Atmospheric sciences (1 work) · Chronology (1 work) · Climate change (1 work) · Climate variability and models (1 work) · Climatology (1 work) · Cloud cover (1 work) · Coastal wetland ecosystem dynamics (1 work) · Daytime (1 work)