N P Molotch
Biographic Data
| ID | 6818976 |
|---|---|
| NAME | N P Molotch |
| GIVEN NAMES | N P |
| FAMILY NAME | Molotch |
| SIGNATURE | MOLOTCH N P |
| AFFILIATIONS | Jet Propulsion Laboratory |
| ORCID | 0000-0003-4733-8060 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 4 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2017 |
| H-INDEX | 0 |
Different sensitivities of snowpacks to warming in Mediterranean climate mountain areas
López-Moreno, Juan I. et. al.- 10 páginas.- Ilustraciones.- This article is an open access article distributed under the terms of the Creative Commons Attribution 3.0 licence (https://creativecommons.org/licenses/by/3.0/)
Impacts of increasing aridity and wildfires on aerosol loading in the intermountain Western US
Feedbacks between climate warming, land surface aridity, and wildfire-derived aerosols represent a large source of uncertainty in future climate predictions. Here, long-term observations of aerosol optical depth, surface level aerosol loading, fire-area burned, and hydrologic simulations are used to show that regional-scale increases in aridity and resulting wildfires have significantly increased summertime aerosol loading in remote high elevatio…
Topoclimate effects on growing season length and montane conifer growth in complex terrain
Spatial variability in the topoclimate-driven linkage between forest phenology and tree growth in complex terrain is poorly understood, limiting our understanding of how ecosystems function as a whole. To characterize the influence of topoclimate on phenology and growth, we determined the start, end, and length of the growing season (GS(start), GS(end), and GSL, respectively) using the correlation between transpiration and evaporative demand, mea…
Energy budget increases reduce mean streamflow more than snow–rain transitions: Using integrated modeling to isolate climate change impacts on Rocky Mountain hydrology
In snow-dominated mountain regions, a warming climate is expected to alter two drivers of hydrology: (1) decrease the fraction of precipitation falling as snow; and (2) increase surface energy available to drive evapotranspiration. This study uses a novel integrated modeling approach to explicitly separate energy budget increases via warming from precipitation phase transitions from snow to rain in two mountain headwaters transects of the central…
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Energy budget increases reduce mean streamflow more than snow–rain transitions: Using integrated modeling to isolate climate change impacts on Rocky Mountain hydrology
In snow-dominated mountain regions, a warming climate is expected to alter two drivers of hydrology: (1) decrease the fraction of precipitation falling as snow; and (2) increase surface energy available to drive evapotranspiration. This study uses a novel integrated modeling approach to explicitly separate energy budget increases via warming from precipitation phase transitions from snow to rain in two mountain headwaters transects of the central…
Different sensitivities of snowpacks to warming in Mediterranean climate mountain areas
López-Moreno, Juan I. et. al.- 10 páginas.- Ilustraciones.- This article is an open access article distributed under the terms of the Creative Commons Attribution 3.0 licence (https://creativecommons.org/licenses/by/3.0/)
Impacts of increasing aridity and wildfires on aerosol loading in the intermountain Western US
Feedbacks between climate warming, land surface aridity, and wildfire-derived aerosols represent a large source of uncertainty in future climate predictions. Here, long-term observations of aerosol optical depth, surface level aerosol loading, fire-area burned, and hydrologic simulations are used to show that regional-scale increases in aridity and resulting wildfires have significantly increased summertime aerosol loading in remote high elevatio…
Topoclimate effects on growing season length and montane conifer growth in complex terrain
Spatial variability in the topoclimate-driven linkage between forest phenology and tree growth in complex terrain is poorly understood, limiting our understanding of how ecosystems function as a whole. To characterize the influence of topoclimate on phenology and growth, we determined the start, end, and length of the growing season (GS(start), GS(end), and GSL, respectively) using the correlation between transpiration and evaporative demand, mea…
Environmental Science (4 works) · Climate change (3 works) · Geography (3 works) · Geology (3 works) · Meteorology (3 works) · Precipitation (3 works) · Atmospheric sciences (2 works) · Climate model (2 works) · Climatology (2 works) · Cryospheric studies and observations (2 works)