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Climate Engine allows users to analyze and interact with climate and earth observations for decision support related to drought, water use, agricultural, wildfire, and ecology.
The Navajo Nation Drought Severity Evaluation Tool (DSET) is a co-developed cloud-based web application designed to meet the needs of w
These experimental drought blends integrate several key drought monitoring products and indices into a single short-term or long-term product, based on the methodology developed at the NOAA Climate
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In the western U.S., the impacts of drought conditions in the 21st century are increasingly evident as extended fire seasons, dwindling water supplies, and widespread tree mortality are becoming more common occurrences. Fundamentally, drought is a shortage of water that is driven by an imbalance between supply and demand. From a meteorological perspective, periods of low precipitation (i.e., the
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Climate Change and “Atmospheric Thirst” to Increase Fire Danger and Drought in Nevada and California
Since the start of the 21st century, California and Nevada have suffered extreme wildland fires and droughts that have caused devastating impacts to ecosystems and society. A common feature of these events has been very high evaporative demand—the “thirst” of the atmosphere—which has largely been driven by increased air temperatures caused by anthropogenic climate change. According to new
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California and Nevada’s climate and weather patterns create fire-prone environments for many wildland–urban interface communities, highlighting the value in understanding the relationships between drought and wildfire. More specifically, information is needed on how drought indices are related to fire danger outputs that are commonly used in fire management.
With NIDIS Coping with Drought
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In an era of increasing wealth of earth observations, approaches for quickly accessing, analyzing and visualizing environmental data to better inform decision making at relevant scales is needed. Climate Engine enables users to utilize on-demand cloud computing and visualization to analyze and interact with climate and earth observations for decision support related to drought, water
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Drought can have a significant impact on the management and operations of water utilities, from loss of water supply and poor source water quality to increased demand from customers and reduced revenues. Changing conditions in precipitation, snowpack, soil moisture, temperature, and evapotranspiration must be well monitored and better forecasted to provide water managers early warning of drought
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The 2018-2019 water year is now underway, and with all eyes on the developing El Niño, there are many people wondering whether this winter will be any better than last year - particularly for snowpack in the West.
Last winter was marked by below-average precipitation and above-average temperatures through the first several months in many places across the country - with relief not
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The Evaporative Demand Drought Index, also known as EDDI, is an experimental drought monitoring and early warning tool that looks for drought using atmospheric evaporative demand (also known as the “thirst of the atmosphere”). So far, EDDI maps and data have been made available for near-real-time and historical monitoring; now, with the help of the NOAA-National Centers for Environmental
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Written in collaboration with the Western Regional Climate Center (WRCC)
The physical relationship between drought and fire is complex, due to the many and varied first- and second-order effects at national, regional, and local scales. The timing, intensity, and frequency of drought events can have wildly divergent impacts on fuel flammability, fire behavior, and subsequently, wildland fire
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Visit the new snow drought page
The beginning of the 2017/2018 winter season brought little rain and snow, giving rise to concerns about snow drought across the Western United States. Snow drought is defined as a period of abnormally low snowpack for the time of year, reflecting either below-normal cold-season precipitation (dry snow drought) or a lack of snow accumulation, despite near-
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