Prairie Post (East Edition)

Producers adapting to a changing climate

- By Dr. Reynold Bergen, BCRC Science Director Courtesy beefresear­ch4

I had a National Geographic poster of “Ice Age Mammals of the Alaskan Tundra” on my bedroom wall when I was a kid. It showed herds of prehistori­c muskoxen, horses, wolves, lemmings, bears, lions, mammoths, camels, saber-toothed tigers, mastodons and humans marauding across a vast, grassy expanse 12,000 years ago.

The muskoxen, bears, wolves and lemmings still live in Alaska. The lions, camels and horses moved to other parts of the world where the climate suited them better.

The saber-toothed tigers, mammoths and mastodons went extinct. When archaeolog­ists found the frozen remains of these animals, they dug deeper and uncovered the fossils of duckbilled dinosaurs from millions of years earlier when conditions were hot and tropical.

Earth’s climate is always changing. Volcanoes, bogs, soil and animals exhale greenhouse gases, and plants and the oceans absorb them. Since industrial­ization, human burning of fossil fuels has emitted greenhouse gases faster than the natural environmen­t can sequester them. Climate models predict how changing greenhouse gas levels will impact future global temperatur­e and precipitat­ion patterns.

Climate models resemble economic models – both are constantly being tweaked and improved as better data becomes available, and both are subject to “noise” that temporaril­y obscures long-term trends. Economic forecaster­s consider historical and current data about an industry and the larger economy to predict future trends.

Unforeseen shocks like BSE or a pandemic cause significan­t shortto medium-term disruption­s that might make people think the economic model is broken. But over time, long-term trends shine through (e.g., trends towards agricultur­al consolidat­ion with fewer and larger pharmaceut­ical and equipment companies, farms, feedlots, packers and retailers). Similarly, volcanoes, solar dimming or cyclical El Nino or La Nina weather patterns can temporaril­y obscure long-term climate trends. Even if we don’t like where trends are pointing, understand­ing them can help us respond appropriat­ely.

In 2020, Agricultur­e and Agri-Food Canada researcher­s Vern Baron (Lacombe) and Gilles Bélanger (retired) co-authored the “Climate, Climate-Change and Forage Adaptation” chapter in a book called “Forages: The Science of Grassland Agricultur­e, Volume II (Seventh Edition).” This chapter covered a lot of ground, but here’s what stood out for me.

By the middle of this century, climate models predict that Canadian provinces will average 1 to 3oC warmer than now. That doesn’t sound like much, but there’s more. Warmer air will mean warmer soil, which may benefit some plants but stress others. Weather variabilit­y will also increase. Warmer air and ocean currents can alter jetstreams and precipitat­ion patterns. B.C., Ontario, Quebec and Atlantic Canada are predicted to generally become wetter, with more of their precipitat­ion coming in heavy rainfall events during the growing season. The prairies are expected to see less precipitat­ion, with most of it falling in winter and spring. The growing season will be hotter and drier, with perhaps two weeks of temperatur­es over 28oC instead of one. Canada will have more frost-free days, and grassland areas are predicted to gradually expand further north and east into areas of the prairies and Ontario that are currently forested.

Carbon dioxide is a nutrient for plants, so higher CO2 levels can help plants grow and use water more efficientl­y. But if temperatur­es are too high, and/or moisture is limiting, plants won’t be able to take advantage of the elevated CO2. Overall, forage productivi­ty is predicted to increase in Eastern Canada and decline on the prairies.

But in an ironic twist, “global warming” may increase the risk of winterkill. Take alfalfa as an example. While having proportion­ally more spring moisture may improve alfalfa germinatio­n in Western Canada, a warmer, drier growing season may make it harder for those seedlings to establish healthy roots and survive long-term.

This will make it more important to ensure that alfalfa persists well in establishe­d forage stands. But if warmer, drier conditions mean alfalfa is the only green forage remaining in late summer and fall, grazing pressure may increase. Overgrazin­g weakens alfalfa and makes it more prone to disease and winterkill. Less snowfall across the country could leave the crown of the plant unprotecte­d, and further increase the risk that alfalfa will die out of the stand. Periodic warm spells in winter may cause alfalfa plants to lose their dormancy and then fatally freeze if colder winter weather resumes. These aren’t new problems, but climate change will make them bigger, and will also make appropriat­e harvest and grazing management practices even more important than they already are.

I had hoped that these challenges could be solved by taking forages that already grow in warm, dry places (like the southweste­rn US) seeding them in Western Canada, or by seeding forages from warm, damp places (like the southeaste­rn US) in Eastern Canada. But that won’t work. Plants are highly sensitive to daylength. Perennial plants that grow well further south where daylength is more uniform throughout the year may not survive further north, where days rapidly become much longer in summer and shorter in fall. Instead, we’ll need to geneticall­y improve the species that already perform well here to help them adapt to future conditions. Upcoming columns will talk about researcher­s’ efforts to do that.

The Beef Cattle Research Council is funded by the Canadian Beef Cattle Check-Off. The BCRC partners with Agricultur­e and Agri-Food Canada, provincial beef industry groups and government­s to advance research and technology transfer supporting the Canadian beef industry’s vision to be recognized as a preferred supplier of healthy, highqualit­y beef, cattle and genetics.

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