Surface ozone in Joshua Tree National Park

2014 ◽  
Vol 87 ◽  
pp. 95-107 ◽  
Author(s):  
Joel D. Burley ◽  
Andrzej Bytnerowicz ◽  
John D. Ray ◽  
Susan Schilling ◽  
Edith B. Allen
Keyword(s):  
National Park ◽  
Surface Ozone ◽  
Joshua Tree National Park

scholarly journals Decadal Trends and Variability in Intermountain West Surface Ozone near Oil and Gas Extraction Fields

2019 ◽  
Author(s):  
Ying Zhou ◽  
Huiting Mao ◽  
Barkley C. Sive
Keyword(s):  
Natural Gas ◽  
National Park ◽  
Oil And Gas ◽  
Surface Ozone ◽  
Gas Production ◽  
Mitigation Strategies ◽  
The Arctic ◽  
Daily Maximum ◽  
Intermountain West ◽  
Emission Reductions

Abstract. Decadal trends in the annual fourth-highest daily maximum 8-hour average (A4DM8HA) ozone (O3) were studied over 2005–2015 for 13 rural/remote sites in the U.S. Intermountain West. No trends were observed in A4DM8HA O3 at two reference sites, which are located upwind of and thus minimally influenced by emissions from oil and natural gas (O&NG) basins. Trends, or a lack thereof, varied widely at other 11 sites in/near O&NG basins resulting from different controlling factors rather than a simplistic, uniform one. The decreasing trends at Mesa Verde (−0.76 ppbv/yr) and Canyonlands National Park (−0.54 ppbv/yr) were attributed to a 37 % decrease in natural gas production in the San Juan Basin and 35 % emission reductions in coal-fired electricity generation, respectively. The decreasing trend (−1.21 ppbv/yr) at Wind Cave National Park resulted from reduced solar radiation due to increasingly frequent precipitation weather. The lack of trends at remaining sites was likely caused by the increasing O&NG emissions and decreasing emissions from other activities. Wintertime O3 stagnant events were associated with the Arctic Oscillation (AO). Box model simulations suggested that both volatile organic compounds (VOCs) and nitrogen oxides emission reductions during negative AO years while VOC emission reductions alone in positive AO years could effectively mitigate high wintertime O3 within the O&NG basins. Our findings suggest that emissions from O&NG extraction likely played a significant role in shaping long-term trends in surface O3 near/within O&NG basins and hence warrant consideration in the design of efficient O3 mitigation strategies for the Intermountain West.

scholarly journals Hydrological Analysis for Infrastructure Planning and Development at the North Entrance Joshua Tree National Park

2020 ◽  
Author(s):  
◽  
Erick Nyangari
Keyword(s):  
Surface Runoff ◽  
Mojave Desert ◽  
National Park ◽  
Flash Floods ◽  
Desert Region ◽  
The North ◽  
Joshua Tree National Park ◽  
Risk Areas ◽  
Development Plans ◽  
High Flood

Rains in the Mojave Desert region are intense and result in the destruction of property. This destruction is significant and affects development plans in the area. Joshua Tree National Park (JTNP) is one of the areas affected as a result of flash floods in the Mojave Desert region. As part of the efforts to minimize the effects caused by flash floods in the park, there was a need to carry out a hydrological analysis of surface runoff in order to map out high risk areas that are susceptible to floods after Monsoonal rains, identify areas in the park that require diversion berms, and establish the effectiveness of the existing diversion berms. The analysis result was a 3D topographic model and a map that contains high flood risk areas and potential areas where diversion berms may be constructed to divert surface runoff and protect the park’s infrastructure.

scholarly journals LANDSCAPE VALUES OF JOSHUA TREE NATIONAL PARK

space&FORM ◽  
2017 ◽  
Vol 2017 (30) ◽  
pp. 279-294
Author(s):  
Alicja Świtalska ◽  
Keyword(s):  
National Park ◽  
Landscape Values ◽  
Joshua Tree National Park

scholarly journals Supplemental Material: Testing models of Laramide orogenic initiation by investigation of Late Cretaceous magmatic-tectonic evolution of the central Mojave sector of the California arc

2021 ◽  
Author(s):  
R.C. Economos ◽  
et al.
Keyword(s):  
Inductively Coupled Plasma ◽  
National Park ◽  
Granitic Rocks ◽  
Trace Element Geochemistry ◽  
Element Geochemistry ◽  
Inductively Coupled ◽  
Joshua Tree National Park ◽  
Icp Ms ◽  
Plasma Mass Spectrometry ◽  
Shrimp Zircon

<div>Table S1: SHRIMP zircon U-Pb geochronology data for six samples from the Cadiz Valley batholith. Table S2: SHRIMP zircon U-Pb geochronology data for six samples from the Federal 2-26 Cajon Pass drill core. Table S3: Whole-rock major- and trace-element geochemistry of granitic rocks from Joshua Tree National Park and the Cadiz Valley batholith measured by X-ray fluorescence (XRF) and inductively coupled plasma–mass spectrometry (ICP-MS). Table S4: Rb/Sr and Sm/Nd isotope data from the Joshua Tree National Park and Cadiz Valley batholith. Table S5: Locations, data, and references used to generate histograms in Figure 5.<br></div>

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