This section provides expert documentation for users seeking to understand how climate data is structured, stored, and organized on Wy-Adapt. It is designed for users of all technical backgrounds, from those exploring climate data and projections for the first time to experienced analysts seeking a refresher on best practices. Whether you are exploring available datasets, learning how climate projections are developed, or writing code to access data directly from the cloud, these pages provide the technical foundation and practical guidance needed to confidently navigate, analyze, and interpret climate data on Wy-Adapt.
Climate Model Simulations
This section introduces the sources and science behind Wy-Adapt's tools and datasets, including the basics of climate modeling, emissions scenarios, spatial resolution, climate variables, and additional information about the models used. Wy-Adapt provides climate projections - estimates of potential future climate conditions rather than forecasts for specific days. Unlike weather, which describes atmospheric conditions over days or weeks, climate reflects long-term patterns and statistics measured across decades. These projections help users explore how typical conditions and extreme events may change over time, such as warmer July temperatures, shifts in winter snow accumulation, or changes in the frequency and intensity of heat waves and heavy rainfall. Although they cannot predict exactly when an individual event will occur, they can estimate how its likelihood may change in a warming climate. Together, these resources provide a foundation for interpreting climate projections appropriately and using Wy-Adapt to explore possible future climate conditions.
Data Structure and Format
This section explains how data in Wy-Adapt is organized and stored. It introduces the main file types used, explains when and why each type is used, and provides an overview of how the data is organized.
Metadata Standards
This section explains how metadata is used to describe and document the climate data available through Wy-Adapt. It covers the information needed to understand where data comes from, what it represents, and how it should be interpreted and used. Standardized metadata helps ensure that Wy-Adapt datasets are consistent, discoverable, and accessible across different tools and applications.
Wy-Adapt hosts climate data and related information designed to help users understand how the western United States climate may change over time and what those changes may mean for communities, natural resources, and decision-making. The data available through Wy-Adapt is organized to make it easier for users to find, access, and work with the information they need. This section provides an overview of how data within Wy-Adapt is organized and stored. It introduces the primary file formats used by the platform and explains when and why each format may be used.
Wy-Adapt brings together 25 global climate models (GCM’s) selected to provide useful information about the Western United States current and future climate conditions. The climate models included in the platform were evaluated based on how well they represent important aspects of the climate and are suitable for examining potential changes across the country.
The 25 GCMs used are available to explore future climate projections with built-in assumptions. It is recommended to use multiple GCMs to capture the full range of possibilities.
GCMs Used:
GCM | Variant | Description |
access-cm2 | r5i1p1f1 | Commonwealth Scientific and Industrial Research Organization (CSIRO) and Bureau of Meteorology (BOM) Australia |
canesm5 | r1i1p2f1 | Canadian Centre for Climate Modelling and Analysis |
cesm2 | r11i1p1f1 | Community Earth System Model Contributors |
cesm2-le | 1011 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1151 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1031 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1071 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1131 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1171 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1051 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1091 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1191 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cesm2-le | 1111 | The Community Earth System Model Version 2 Large Ensemble (CESM2-LE) is a comprehensive climate modeling project developed collaboratively by the National Center for Atmospheric Research (NCAR) and the IBS Center for Climate Physics in South Korea. |
cnrm-esm2-1 | r1i1p1f2 | Centre National de Recherches Météorologiques/ Centre Européen de Recherche et Formation Avancée en Calcul Scientifique |
ec-earth3 | r1i1p1f1 | EC-Earth consortium |
ec-earth3-veg | r1i1p1f1 | EC-Earth consortium |
fgoals-g3 | r1i1p1f1 | Chinese Academy of Sciences |
giss-e2-1-g | r1i1p1f2 | Goddard Institute for Space Studies |
miroc6 | r1i1p1f1 | Atmosphere and Ocean Research Institute (The University of Tokyo), National Institute for Environmental Studies, and Japan Agency for Marine-Earth Science and Technology |
mpi-esm1-2-hr | r3i1p1f1 | Max Planck Institute for Meteorology |
mpi-esm1-2-hr | r7i1p1f1 | Max Planck Institute for Meteorology |
mpi-esm1-2-lr | r7i1p1f1 | Max Planck Institute for Meteorology |
noresm2-mm | r1i1p1f1 | Norwegian Earth System Model |
taiesm1 | r1i1p1f1 | Research Center for Environmental Changes, Academia Sinica (Taiwan) |
ukesm1-0-ll | r2i1p1f2 | Met Office, Hadley Centre (UK) |
Wy-Adapt climate data are provided at a 9 km spatial resolution, meaning the data are organized into grid cells that are approximately 9 kilometers by 9 kilometers. This resolution provides a useful balance between geographic detail and the computational resources needed to process and analyze climate projections. Data within each grid cell represents the climate conditions for that area, allowing users to examine how projected changes may vary across different areas.
The 9 km grid provides more localized information than coarser-resolution climate datasets while maintaining consistent coverage across the country. Users should keep the grid-cell size in mind when interpreting the data, particularly when comparing climate projections with information about specific communities, watersheds, or other smaller geographic areas.
The Warm Refuge scenario represents a mid-century future in which the globe has warmed approximately 3.6°F (2°C) since the late 19th century. While precipitation increases slightly, warmer temperatures cause more fall and spring precipitation to occur as rain rather than snow. This results in a greater likelihood of low-snow years, even though overall precipitation is slightly higher. The Shrinking Snowpack scenario also represents approximately 3.6°F (2°C) of global warming by mid-century, but with slightly lower precipitation. The combination of warmer and drier conditions substantially increases the likelihood of low-snow years, while rain-on-snow events may contribute to increased flooding. The Hot and Smoky scenario represents a higher-warming future, with approximately 5.4°F (3°C) of global warming by mid-century. Under this scenario, precipitation becomes more variable, while warmer temperatures contribute to earlier spring snowmelt, increased evaporation, and reduced late-summer streamflows. Rain-on-snow events and rapid spring runoff may increase flood risk, while more smoky days during the summer illustrate how multiple climate-related impacts could occur together.
Different climate scenarios use different combinations of Global Climate Models (GCMs) to represent a range of possible future climate conditions. The tables below summarize which GCMs are available for each scenario and provide information to help users understand the differences between them. These scenarios are not predictions of a single future but represent different possible climate conditions that can help illustrate how Wyoming’s climate may change and what those changes could mean for communities, ecosystems, water resources, and other areas of interest.
Scenario | Variant | Description |
Shrinking Snowpack | p50 | Shrinking Snowpack Scenario contains EC-Earth3, GISS-E2-1-G, MIROC6, MPI-ESM1-2-LR, TaiESM1, CESM2-LE_1111, CESM-LE_1191 |
Hot and Smoky | p50 | Hot and Smoky Scenario contains CESM2, EC-Earth3, GISS-E2-1-G, TaiESM1, UKESM1-0-LL, CESM2-LE_1071, CESM2-LE_1111 |
Warm and Refuge | p50 | Warm Refuge Scenario contains CanESM5, EC-Earth3-Veg, FGOALS-G3, MPI-ESM1-2-HR-r3, MPI-ESM1-2-HR-r7, CESM2-LE_1011, CESM2-LE_1131 |
Wy-Adapt climate datasets use a consistent geographic grid to represent climate conditions across the Western United States. Each grid cell has an associated geographic location that allows the climate data to be aligned with maps, geographic boundaries, and other spatial datasets.
The climate datasets available through Wy-Adapt are designed to support analysis of historical and projected climate conditions across the Western United States. Each dataset represents specific climate variables, time periods, and future conditions and can be used to examine how climate may change across different locations and timeframes.
When selecting data, users should consider the purpose of their analysis and choose datasets that match the geographic area, climate variable, time period, and scenario needed for their application. Because climate projections represent a range of plausible future conditions, examining multiple models and scenarios can provide a more complete understanding of potential changes and uncertainty.
The Data Catalog provides additional information about individual datasets, including the variables, time periods, scenarios, models, and other characteristics associated with each dataset.
WY-Adapt provides many different climate variables for users to explore, including frost days, precipitation as snow, and minimum temperature. Each variable represents a different aspect of the Earth's climate and helps users understand how climate conditions may vary across locations and over time. By examining these variables, users can better assess climate trends and their potential impacts on natural and human systems.
Category | Variable | Description |
Precipitation | Total Precipitation | Total amount of water that falls from the atmosphere as rain, snow, or other forms of precipitation during a specified period. Higher precipitation can mean wetter conditions and increased water availability, while lower precipitation can contribute to dry conditions and water shortages. |
Snow | Precipitation as Snow | Amount of precipitation falls as snow during a specified period. This data people understand winter conditions and the amount of precipitation that may contribute to seasonal snowpack. |
Snow | Maximum Annual Snow Water Equivalent | Highest total amount of water contained in the snowpack during a year, also known as snow water equivalent (SWE). A higher SWE indicates more water stored in the snowpack, which can provide a greater water supplies when the snow melts but may also contribute to increased runoff. |
Snow | Percent of Precipitation as Snow | Percentage of total precipitation that falls as snow. This can help show whether an area is receiving more of its precipitation as snow or rain. |
Snow | Snow | Total amount of water contained within the snowpack during a specified month. This helps track how much water is being stored throughout the winter and when the snowpack beings to accumulate or decline. It can be useful in recreation, agriculture, and ecosystem management. |
Snow | Water Year Day of Max Annual Snow Water Equivalent | Calendar Day within a water year when the snowpack contains its highest total amount of water. This indicates when the snowpack reaches its annual peak and can help show whether peak snowpack is occurring earlier or later in the water year. |
Temperature | Average Temperature | Mean temperature recorded over a specified period of time. Average temperature provides a general picture of the climate conditions experienced in an area. |
Temperature | Maximum Temperature | Highest temperature recorded over a specified period of time. This helps identify the hottest conditional an area experience. It can be useful for assessing heat stress, planning for energy demand, managing crops and livestock and understanding impacts on ecosystems. |
Temperature | Minimum Temperature | Lowest temperature recorded over a specified period of time. Minimum temperature helps identify the coldest conditions an area experiences. |
Temperature | Frost Days | Annual number of days when the minimum temperature is less than 32°F (0°C). Frost days are important for agriculture and gardening because freezing temperatures can damage or kill sensitive plants. This information can also help identify changes in growing seasons and frost risk. |
Temperature | Forst Free Periods | Measure the local growing season by counting the parts of the year where the odds of frost are low. Gardeners use this to pick plants that mature before the cold returns. |
Temperature | Growing Degree Days (5°C) | Measures the amount of heat accumulated over time by an organism or crop. Growing Degree Days (GDD), calculated as the cumulative number of daily degrees above 5°C, help predict when plants will emerge, flower, or reach harvest maturity. By reflecting weather conditions, GDD helps farmers and gardeners make more informed management decisions. |
Temperature | Icing Days | Annual number of days when the highest recorded temperature does not exceed 32°F. These are days when temperatures remain at or below freezing throughout the day. Icing days can affect roads, transportation, infrastructure, agriculture, and daily activities and can help indicate the severity and persistence of winter conditions. |
Temperature | Monthly Maximum of Daily Temperature | Average of the daily maximum temperatures within a month. This shows the typical daytime high temperature for each month. Farmers, gardeners, energy planners, and outdoor recreation managers can use this information to understand seasonal heat conditions and how they may change over time. |
Temperature | Monthly Minimum of Daily Temperature | Average of the daily minimum temperatures within a month. This shows the typical nighttime or early-morning low temperature for each month. It can help farmers and gardeners understand frost risk, help communities plan for heating needs, and provide insight into changes in overnight temperatures. |
Extreme Precipitation | Annual Count Precipitation >=20mm/day | Number of days in a year when daily precipitation is greater than or equal to 20 mm. This helps identify how frequently heavy precipitation events occur. Communities and emergence managers can use this information when considering flood risk, stormwater management, and infrastructure needs. |
Extreme Precipitation | Annual Maximum 1-day Precipitation | Highest amount of precipitation recorded within a single day. This helps identify the most intense one-day precipitation event expected in a year. |
Extreme Precipitation | Annual Max 5-day Precipitation | Highest amount of precipitation recorded within a 5-day period. This helps identify periods when large amounts of precipitation accumulate over serval days. |
Extreme Precipitation | Annual Total Precipitation When Daily >95th | Total annual precipitation occurring on days when daily precipitation exceeds the 95th percentile of baseline wet days. This shows how much of the year's precipitation comes from unusually wet events. It can help communities and water managers understand whether precipitation is becoming more concentrated in heavy events rather than being spread more evenly throughout the year. |
Extreme Precipitation | Maximum Consecutive Days Precipitation < 1 mm/day | Maximum number of consecutive days with precipitation less than 1 mm per day. Longer periods can indicate extended dry conditions and may contribute to drought, reduced soil moisture, increased irrigation needs, and stress on crops and vegetation. |
Extreme Precipitation | Maximum Consecutive Days Precipitation > 1 mm/day | Maximum number of consecutive days with precipitation greater than 1 mm per day. Longer wet periods can lead to saturated soils, increased runoff, flooding, and challenges for agriculture, construction, and transportation. |
Extreme Precipitation | Simple Precipitation Intensity Index | Annual average precipitation intensity on days with more than 1 mm of precipitation. This helps show how heavily precipitation falls when it occurs. Higher intensity can result in more rapid runoff and may increase the potential for flooding, erosion, and soil loss.. |
Extreme Temperature | Annual Days Heat Index 80–90°F | Number of days each year when the heat index reaches the 80–90°F caution range. The heat index accounts for both temperature and humidity to describe how hot conditions feel to the human body. This information can help communities, outdoor workers, event planners, and public health officials identify periods when additional heat precautions may be needed. |
Extreme Temperature | Annual Days Heat Index 90–105°F | Number of days each year when the heat index reaches the 90–105°F extreme caution range. More days in this range indicate increased exposure to potentially hazardous heat. |
Extreme Temperature | Annual Days Heat Index 105–130°F | Number of days each year when the heat index reaches the 105–130°F danger range. These conditions represent dangerous heat that can place significant stress on the human body. Communities and public health officials can use this information when planning for heat emergencies, cooling centers, outdoor activities, and worker safety. |
Extreme Temperature | Annual Days Heat Index Over 130°F | Number of days each year when the heat index exceeds 130°F, indicating the extreme danger range. These conditions represent exceptionally severe heat and can pose serious risks to human health. Information about these events can help communities prepare for extreme heat emergencies and identify areas that may need additional resources or planning. |
Extreme Temperature | Annual Days Maximum Temperature >85°F | Number of days in a year when the maximum temperature is higher than 85°F.This provides an indication of how often an area experiences warm or hot days. |
Extreme Temperature | Annual Days Maximum Temperature >90°F | Number of days in a year when the maximum temperature is higher than 90°F. More days above 90°F indicate more frequent hot conditions. This information can help communities, employers, farmers, and public health officials prepare for increased heat exposure, water demand, and energy use. |
Extreme Temperature | Annual Days Maximum Temperature >95°F | Number of days in a year when the maximum temperature is higher than 95°F. This indicates how frequently an area experiences very hot days. It can be useful for evaluating heat stress, crop and livestock impacts, energy demand, water use, and the need for heat preparedness. |
Some climate information available through Wy-Adapt is calculated from one or more underlying climate variables. These calculations produce derived variables or indices that can provide a more useful way of describing climate conditions for a particular application.
Derived variables are created by applying a calculation to existing climate data. For example, multiple temperature measurements may be combined to describe conditions over a particular period. Climate indices take this a step further by combining climate variables into a measure that can help describe a specific impact or condition.
Because derived variables and indices depend on the underlying data and calculation method, users should review the definition, units, and methodology associated with each measure before using it in an analysis.
Climate models do not perfectly reproduce observed climate conditions, and the differences between modeled and observed data are known as bias. Bias can vary by location, season, and climate variable. For WY-Adapt researchers found that biases in the global climate model could lead to unrealistic precipitation and snowfall when the data were used in a higher-resolution regional model (WRF).
To reduce these biases, they corrected the global climate model data before using it to drive WRF. They compared the model's historical climate conditions with a more realistic observational/reanalysis dataset and adjusted the model data to better match the observed conditions. In simple terms, they removed the average difference between the model and observations before running the regional model. This helped prevent the original errors from being amplified during downscaling and produced more realistic precipitation and snow simulations.
Bias correction can therefore make climate model data more useful for certain applications, but it does not eliminate uncertainty in future climate projections. The corrected data should still be interpreted with an understanding of the limitations and uncertainties of the climate models.
Bias correction paper:
Rahimi, S., Huang, L., Norris, J., Hall, A., Goldenson, N., Risser, M., Feldman, D. R., Lebo, Z. J., Dennis, E., & Thackeray, C. (2024). Understanding the Cascade: Removing GCM Biases Improves Dynamically Downscaled Climate Projections. Geophysical Research Letters, 51(9), e2023GL106264. https://doi.org/10.1029/2023GL106264
Wy-Adapt provides access to climate projection data developed to help users explore potential changes in Wyoming’s climate. The data are organized so that users can work with climate variables across different time periods, locations, and climate scenarios. Wy-Adapt uses a consistent 9 km grid across the state, allowing projected climate conditions to be compared across geographic areas. The platform also provides tools and documentation to help users understand the available datasets and determine which data are appropriate for their analysis.
The climate data available through Wy-Adapt are organized around several key characteristics, including climate variable, time period, climate scenario, and geographic location. Climate variables describe the specific aspect of climate being analyzed, such as temperature or precipitation, while scenarios represent different possible future climate conditions. Data are provided on a 9 km grid, with each grid cell representing the climate conditions for a specific area of Wyoming.
This structure allows users to select the information most relevant to their needs rather than working with an entire dataset at once. For example, a user may be interested in a particular climate variable, future scenario, and time period for a specific area of Wyoming. The Wy-Adapt tools and data documentation provide guidance for identifying and working with these combinations of data.
Climate datasets may be provided in formats designed for both analysis and data sharing. Common climate data formats include NetCDF and Zarr, which are capable of storing multi-dimensional data such as climate variables across time and geographic locations.
NetCDF files store climate data in a single file and are widely used for sharing and analyzing scientific datasets. They can be useful when working with a manageable portion of a dataset or when a complete file is needed for local analysis. However, large climate datasets can require substantial computer memory and storage when opened or downloaded in their entirety.
Zarr is designed for working with large, multi-dimensional datasets and is particularly well suited for cloud-based analysis. Rather than requiring an entire dataset to be downloaded before it can be analyzed, Zarr allows users to access portions of the data as needed. This can make it more efficient to work with large climate datasets covering many years, variables, and geographic locations.
The way Wy-Adapts data is organized allows users to move from broad exploration of available climate information to more targeted analysis. Users who are working through the Wy-Adapt interface can explore climate projections without directly interacting with the underlying data structure, while more advanced users can use the documented data access methods to work directly with the datasets.
For information about the climate models, scenarios, variables, and spatial resolution represented in Wy-Adapt, see the Climate Model Simulation section. For guidance on finding and accessing specific datasets, see the Developer API and Data Brower sections.
Metadata is information that describes a dataset and helps users understand what the data represents, where it came from, and how it can be used. Wy-Adapt follows standard metadata practices to make climate data easier to understand, share, and use across different tools and platforms.
Readability
Standard conventions organize information in a consistent format that can be understood by both people and computer software. This makes datasets easier to interpret and work with.
Interoperability
Using established standards allows Wy-Adapt data to work with common scientific, geographic, and data analysis tools. Standardized datasets can also be combined with information from other sources with less additional processing.
Data Access
Consistent formats and metadata make it easier for users to discover, download, and analyze Wy-Adapt data. This is especially important for large climate datasets that may be accessed through different software and programming environments.
Documentation
Datasets should provide enough information for users to understand what they contain without relying on separate documentation. Metadata should describe the dataset's source, variables, units, time period, spatial information, and other details needed to correctly interpret and use the data.
Climate datasets should include clear descriptions of their variables, units, geographic coordinates, and time information. Where applicable, datasets should follow established standards such as the Climate and Forecast (CF) Conventions for NetCDF data.
At a minimum, metadata should identify:
Dataset title — A clear description of the data.
Source — The model, observations, or other source used to produce the data.
Variables — The climate measurements included in the dataset.
Units — The measurement units for each variable.
Spatial information — The coordinate system and grid used to represent locations.
Time information — The time period and calendar used by the dataset.
Scenario and model information — The climate scenario and GCM associated with the data, when applicable.
Description and references — Information about how the dataset was created and where users can find additional documentation.
Following these standards helps ensure that Wy-Adapt datasets are understandable, discoverable, and usable by both technical and non-technical users.
*To use these citations, please replace the placeholders [] with the specific information from the application, and update the data in both citations with the actual data or retrieval.
To cite visualizations and general information from WY-Adapt like charts, screenshots, ect.:
WY-Adapt. (2023). [Average Temperature for Huc 12 100700070103, Global Climate Models access-cm2, cesm2, ensemble, fgoals-g3]. Wy-Adapt website developed by the Wyoming Geospatial Information Science Center (WyGISC) at the University of Wyoming with funding from the National Science Foundation Grant number OIA-2149105. Retrieved April 24, 2024, from https://wyadapt.org.
How to cite WY-Adapt datasets:
WY-Adapt. (2023). Derived Data GeoTIFF. Data derived from Downscaled CMIP6 Climate Projections. Wy-Adapt website developed by the Wyoming Geospatial Information Science Center (WyGISC) at the University of Wyoming with funding from the National Science Foundation Grant number OIA-2149105. Retrieved April 24, 2024, from https://wyadapt.org.
WUS-D3 overview paper:
Rahimi, S., Huang, L., Norris, J., Hall, A., Goldenson, N., Krantz, W., Bass, B., et al. (2024). An Overview of the Western United States Dynamically Downscaled Dataset (WUS-D3). Geoscientific Model Development, 17(6), 2265–2286. https://doi.org/10.5194/gmd-17-2265-2024
Bias correction paper:
Rahimi, S., Huang, L., Norris, J., Hall, A., Goldenson, N., Risser, M., Feldman, D. R., Lebo, Z. J., Dennis, E., & Thackeray, C. (2024). Understanding the Cascade: Removing GCM Biases Improves Dynamically Downscaled Climate Projections. Geophysical Research Letters, 51(9), e2023GL106264. https://doi.org/10.1029/2023GL106264