SOARS Manuscripts
Papers and posters by protégés in the Significant Opportunities in Atmospheric Research (SOARS) program, dating back to the program's start in 1996.
Displaying 126–150 of 501 results
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Tropical cyclones (TCs) that develop in the southwest Caribbean Sea (SWCS) commonly make landfall due to their relatively close proximity to land masses, bringing flooding rains, high winds, and destructive storm surge to the impacted areas. Despite the dangers posed by SWCS TCs, there are relativel…
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Exploring the synoptic differences between MJO initiation events identified by multiple algorithms(opens in new tab)
The Madden-Julian Oscillation (MJO) is a tropical phenomenon developing over the Indian Ocean. This intraseasonal oscillation involves an extensive area of convection, approximately 1000 km across, releasing latent heat in the mid-troposphere. This heating generates planetary-scale waves that travel… -
Small-scale spatial variability of ozone in Boulder, Colorado(opens in new tab)
Surface ozone (O3) is detrimental and can pose several health problems to humans, such as increased number of and intensity of asthma attacks. Considering this, it is important that these ozone levels be monitored. While municipal air quality monitors are present in cities like Boulder, Colorado, th… -
Links between the Hadley Circulation and Oxygen Minimum Zones(opens in new tab)
This research aimed to find links between the projected changes in oceanic oxygen minimum zones (OMZs) and the Hadley Circulation (HC). OMZs are regions of very low oxygen concentrations. Latitudinal ocean oxygen slices place the OMZs in the eastern edges of ocean basins. Recent research suggests th… -
Modification of a tropical storm tracking algorithm for extra-tropical cyclone detection(opens in new tab)
Extra-tropical cyclones are the main source of weekly weather variability across much of the middle latitudes and are often associated with damaging winds, coastal erosion, and significant precipitation. Under the right dynamic and thermodynamic conditions, these cyclones may rapidly intensify. This… -
Ingesting geospatial data into Hazard Services' database for National Weather Service flood alerts(opens in new tab)
Statistically, flooding is the most devastating natural disaster not only in the US, but in the world. Of the many different severe and normal weather events, floods typically cause the most casualties and damage. Within Hazard Services of the National Oceanic and Atmospheric Administration, softwar… -
Utilizing portable air quality monitors to assess the patterns of ozone along the northern Front Range of Colorado(opens in new tab)
High levels of ozone in the troposphere are recognized to produce a myriad of harmful effects on human health. Due to significant interest in the quality of air along the Front Range in Colorado, the Front Range Air Pollution and Photochemistry Experiment (FRAPPÉ) launched a field campaign utilizing… -
North Atlantic amospheric blocking and Atlantic multidecadal oscillation in CESM1 large ensemble simulations(opens in new tab)
Atmospheric blocking is an unusual weather phenomenon that is often associated with severe weather events such as heat waves, cold spells, and droughts. Improved understanding of the long-term variability of atmospheric blocking has important societal implication, but its mechanisms are not well und… -
Understanding the 2013 Boulder Flood: Assessing extreme precipitation events and future climates in the Community Earth System Model (CESM)(opens in new tab)
The Boulder flood of September 2013 resulted in significant structural damage, inundated communities, and accelerated land erosion in central and northern Colorado. Approximately 11,000 people were evacuated in the area as more than 17 inches of rain fell in parts of Boulder County, Colorado in 7 da… -
Effects of large volcanic eruptions on climate in the Community Earth System Model(opens in new tab)
This research investigated the climate system's response to large volcanic eruptions in the Community Earth System Model-Large Ensemble (CESM-LE). Using 29 CESM-LE global simulations with each ensemble member having a unique prediction about the weather and how climate will change; the climate syste… -
Using the Mesoscale Model Evaluation Testbed (MMET) to test physics options in the Weather Research & Forecasting (WRF) model(opens in new tab)
The Mesoscale Model Evaluation Testbed (MMET) has been established by the Developmental Testbed Center (DTC) to assist the research community in efficiently testing and evaluating newly developed model techniques aimed at more accurately predicting the weather and potentially implementing them into … -
Innovating the future: Engineering sustainable cooking technologies in north Ghana for improved air quality(opens in new tab)
Over half of the world's population in developing nations heat their homes and cook using open fire or cookstoves fueled by solid biofuels. The emissions generated from the burning of biofuels have the potential to have a significant impact on human health, air quality, and the regional and global c… -
Sensitivity of a simulated squall line to the microphysical representation of Graupel(opens in new tab)
In order to accurately simulate storms and their precipitation within atmospheric models, we need to ensure that atmospheric processes are well parameterized. In the case of the Thompson microphysics parameterization, the rain, snow, cloud drop, cloud ice and graupel/hail hydrometeor categories have… -
Observations of wind asymmetries in Atlantic tropical cyclones(opens in new tab)
Most major cities are located on coastlines, vulnerable to the direct impacts of tropical cyclones. Therefore, it is critical to understand and improve the prediction of these storms in order to make communities more resilient. Though hurricane warning systems have improved in recent years, these wa… -
Three-dimensional variation of atmospheric CO₂: A comparison of aircraft measurements with inverse model simulations(opens in new tab)
Accumulation of CO2 impacts climate resulting in an increase of global temperatures. It is vital to know the underlying processes driving the uptake of CO2 emissions by the biosphere and oceans to infer the rate at which CO2 concentrations will increase in the atmosphere. In this paper, we compare v… -
Evolution of phytoplankton in a changing climate(opens in new tab)
Anthropogenic emissions of greenhouse gases have led to an increase in CO₂ and temperature in the atmosphere, as well as an increase in the sea surface temperature (SST). It has been suggested that a rise in SST leads to an increase in ocean stratification, surface nutrient limitation, and a possibl… -
Using GLOBE student cloud type and contrail data to complement satellite observations(opens in new tab)
The GLOBE Program is a community program of students, teachers, and scientists who collect and analyze Earth Science data to help sustain, understand and improve the earth. In one of the GLOBE projects, students from around the world record and submit cloud type and contrail data online. The purpose… -
Identifying long-range sources of ozone utilizing an adjoint method(opens in new tab)
It has been observed that local ozone concentrations can be impacted by both local emissions and emissions that were transported from distant source regions. Thus, changes in ozone concentration in a particular region can only be understood by analyzing the precursor emission sources, such as nitrog… -
The effect of changes in the Hadley circulation on oxygen minimum zones in the ocean(opens in new tab)
Recent research argued that the Hadley circulation (HC) is composed of three regional cells located at the eastern edges of the ocean basins, rather than a single, globe-encircling cell as the classic textbook view suggests. The HC is expected to expand in concert with global warming, which means th… -
An investigation of evapotranspiration rates within mid-western agricultural systems in response to elevated carbon dioxide and ozone concentrations and climate change(opens in new tab)
Because the human population is expected to surpass 8 billion by the year 2050, food security is a pressing issue. In the face of elevated temperatures and precipitation associated with climate change (CC), elevated carbon dioxide (CO2) and elevated ozone (O3) concentrations, food productivity is un… -
Determining the vertical distribution of volcanic plumes and SO₂ column amounts from 2004-2013(opens in new tab)
The statistics of volcanic eruptions and injections of sulfur dioxide (SO2) into the atmosphere during 2004-2013 are determined using information gathered from the Smithsonian's Global Volcanism Program and the Ozone Monitoring Instrument (OMI), respectively. Volcanic eruptions are observed during t… -
Relating total lightning and storm microphysics to in-cloud convective turbulence(opens in new tab)
Convectively induced turbulence (CIT) has been shown to cause or factor into a large portion of weather-related commercial aviation accidents. Determining areas of CIT is difficult since CIT is a relatively small scale phenomenon. The Federal Aviation Administration issued guidelines for pilots to a… -
Pacific Northwest ecosystem responses to atmospheric changes in the 21st century(opens in new tab)
The terrestrial carbon cycle regulates carbon pools and fluxes throughout the Earth system. Currently, the Pacific Northwest is a carbon sink; it is gaining more carbon than it is releasing into the atmosphere. Investigating changes to this carbon sink is critical for understanding ecosystem respons… -
Evaluation of the planetary boundary layer heights derived from GPS radio occultation soundings over the VOCALS-REx area(opens in new tab)
Earth's planetary boundary layer (PBL) plays an important role in water vapor and heat exchange between the surface and atmosphere through turbulent processes. Using data from the COSMIC/ FORMOSAT-3 global positioning system (GPS) radio occultation (RO) soundings and high-resolution radiosondes laun… -
How the chemical composition of the pre-storm and inflow regions compare to each other and to the outflow region of deep convection in the upper troposphere(opens in new tab)
Ozone in the upper troposphere is considered a greenhouse gas, which can contribute to climate change. Convection in thunderstorms can carry ozone precursors upward from the boundary layer into the upper tropospheric region. Production of nitrogen oxides associated with lightning in the storm can al…