By David I. Gustafson, Adjunct Research Faculty at Washington State University

This article is part of a series, Climate Friendly Fruit & Veggies, highlighting work from the Fruit & Vegetable Supply Chains: Climate Adaptation & Mitigation Opportunities (F&V CAMO) project, a collaborative research study co-led by investigators at the University of Florida and the Agriculture & Food Systems Institute. Other collaborators include researchers at the University of Arkansas, University of Illinois, the International Food Policy Research Institute, the World Agricultural Economic and Environmental Services, and Washington State University. This project seeks to identify and test climate adaptation and mitigation strategies in fruit and vegetable supply chains.

Water. H 2 O. It’s the dominant molecule of our lives. We are 60% water (on average). Life as we know it is only possible because our planet has so much water. We can survive a few weeks without food, but only a few days without water. The oceans are believed to have formed around 4 billion years ago, and so are nearly as old as the planet itself. The hydrologic cycle—the series of processes by which water evaporates from those oceans, condenses as clouds, and then returns to the earth as freshwater—forms the primary basis for our existence.

Figure 1. Comparison of the ‘new normal’ annual precipitation averages (1991-2020) with the previous 30-year averages (1981-2010). Source: NOAA.

Water is actually the most important greenhouse gas: without water in the atmosphere, the average temperature of our planet would be around 0°F… a mammoth version of those chic, spherical ice ‘cubes.’ But the average temperature of the earth is 60°F and climbing. As the world’s oceans continue to warm, water evaporates more rapidly, and the hydrologic cycle accelerates. All that water must come back down somewhere, so annual precipitation levels across the planet are also increasing. Continue reading →

By Nicole Bell, Center for Sustaining Agriculture and Natural Resources, Washington State University

Heat wave damage to a commonly grown blackberry cultivar, Columbia Star (photo taken July 1, 2021). Photo courtesy of Dr. Bernadine Strik.

It wasn’t just hot in the Pacific Northwest (PNW) during the last week of June. It was extraordinarily hot. Temperatures at Oregon State University’s North Willamette Research and Extension Center (NWREC) in Aurora, Oregon, reached a high of 113°F on June 28, with a nighttime low of 85°F. It wasn’t just one day of scorching temperatures, though—much of the PNW experienced more than three consecutive days of highs in the triple digits, with lows staying above 65°F. With temperatures peaking in Lytton, British Columbia, Canada, at 121°F, some outlets are calling this multi-day event a heat dome. Growers are feeling the impact of June’s high temperatures. How does this type of heat affect staple and specialty crops, and how can the agricultural industry in the Pacific Northwest best prepare for events like this to come? Read on for some insights from the June heat dome.

A wide variety of crops were impacted by the record-setting heat, notably berries, cherries, and even some vegetables across the region. Continue reading →

By Sonia A. Hall

Fire danger was considered extreme on and around Labor Day 2020. Close to the Beachie Fire in Marion County, OR. Photo: Oregon Department of Transportation, under CC BY 2.0.

Most of us probably agree that 2020 was an unprecedented year in many ways. Much of the western U.S. will remember 2020 for, among other things, the extensive fires that burned across many states. One of those states is Oregon, where climatic and weather conditions converged during Labor Day to enable large fires across the western slopes of the Cascades. Check out climatologists John Abatzoglou, David Rupp, and Larry O’Neill’s article titled Climate Enabling Conditions and Drivers of the Western Oregon Wildfires of 2020. They discuss the conditions that enabled these fires, and provide some historical context for their occurrence. Spoiler alert: their concluding paragraph states that “The best science available indicates that the conditions that enable large wildfires and wildfire seasons will become more common as a result of climate change and past and current land management and land use.” Many communities are heeding this information and working towards reducing vulnerabilities and improving resilience, to better deal with future fires. Please share with us and AgClimate.net readers those tools, resources and information you have found useful in such efforts.  You can comment on this post, or contact us via the Ask A Question tab.

By Paris Edwards

Headwater streams originate in mountainous areas and add critical snowmelt to summer and early fall stream flows. Slow and steady melt off of winter snowpack provides water during the dry season when crops need it most. Photo by Picasa, Wikimedia Commons under CC BY-SA 3.0.

Our understanding of regional climate change effects today will be used to inform management, policy, and the new scientific endeavors of tomorrow. With this in mind, a team of doctoral students from the Water Resources Department at the University of Idaho in Moscow carried out a systematic review of all peer-reviewed studies through 2016 (550 of them) related to climate change in headwater regions of the Columbia River Basin. The purpose of the review was to explore what aspects of climate change impacts on water availability have been well studied, and where additional research is still needed (Marshall et al. 2020). We focused on mountain headwater regions because these critical water-generating areas are vulnerable to increasingly warm winter temperatures that contribute to snowpack losses and increased variability in the timing and volume of water available for multiple uses. Water availability supports values we care about and communities in our region, including irrigation; the future of irrigated agriculture in the Basin depends on water, and at least 20% of surface supply in the Basin is generated from melted snow. Continue reading →