Spring 2022 Weather Outlook

Spring 2022 Temperature Outlook
Spring 2022 Temperature Outlook

March - May 2022 National Temperature Outlook Source: NOAA Climate Prediction Center

Spring 2022 Temperature Outlook

Spring 2022 Precipitation Outlook
Spring 2022 Precipitation Outlook

March - May 2022 National Precipitation Outlook Source: NOAA Climate Prediction Center

Spring 2022 Precipitation Outlook

Subsurface Equatorial Pacific Temperature Anomalies
Subsurface Equatorial Pacific Temperature Anomalies

60-day Subsurface Heat Content for the Equatorial Pacific Source: NOAA Climate Prediction Cente

Subsurface Equatorial Pacific Temperature Anomalies

Climate Prediction Center Spring Outlook

The Climate Prediction Center (CPC) released the equivalent of their Spring outlook yesterday, along with their rolling 3-month outlooks through the March-May 2023 period for temperatures and precipitation. The temperature and precipitation outlooks for the next three months can be viewed in Figures 1 (temperature) and Figure 2 (precipitation).

From CPC’s perspective, most areas east of the Rocky Mountains are forecast to see above normal temperatures, with the highest probability of occurrence odds assigned to the southwestern half of Texas and the southeastern quarter of New Mexico. The only area of the continental United States that is favored to receive below normal temperatures includes the northwestern ½ of Oregon, all of Washington, the northern 1/3 of Idaho and the northwestern 1/3 of Montana.

Nebraska lies on the northern periphery of the above normal temperature forecast with odds slightly tilted toward these conditions. The entire state has been assigned a 33-40% chance of above normal temperatures, 33% of normal temperatures, and a 26-33% chance of below normal temperatures.

Above normal precipitation over the next three months is projected to occur across the Ohio River Valley and the northwestern United States. However, a dry signal is indicated for the western half of the central and southern High Plains region, with the highest probability of occurrence assigned to the four corners region of the United States (CO, UT, NV, NM). CPC has assigned a 50-60% probability that this region will experience below normal moisture, with a 33% chance of normal precipitation and a 7-17% chance of above normal moisture.

Delving deeper into the Nebraska outlook, CPC indicates the southern ¾ of the Panhandle, the western Sandhill region and southwest Nebraska have been assigned a 40-50% probability of below normal moisture. The odds for normal moisture is 33%, with a 17-27% chance of above normal moisture. The northern Panhandle and the central 1/3 of Nebraska have been assigned a 33-40% chance of below normal moisture, 33% chance of normal moisture and a 27-33% chance of above normal moisture. For the remainder of the state, CPC has assigned equal odds (33% chance) of receiving normal, above normal or below normal precipitation.

If CPC’s forecast verifies, drought conditions across the western half of the state will intensify due to the lack of subsoil moisture recharge and a poor finish to the snowpack season across northern Colorado. Conversely, the strong signal for above normal moisture in the Ohio River valley would intensify wetness concerns dating back to last fall. Much of this region has received 10-18 inches of moisture since the beginning of last October.

My Thoughts on CPC’s Outlook

To be blunt, if CPC’s temperature and precipitation outlook for the next 3 months were to verify, drought conditions across western Nebraska would intensify rapidly. The western 2/3 of the state missed out on the October precipitation events that hit eastern Nebraska and the dry conditions this winter have only intensified the lack of subsoil moisture recharge. In fact, the dryness this winter has eliminated the surplus precipitation that eastern Nebraska received last fall. Without normal moisture this spring, areas of eastern Nebraska currently depicted as abnormally dry by the U.S. Drought Monitor would be expected to see moderate drought conditions develop before the end of this Spring.

The lack of snowfall this winter has provided producers ample opportunity to do field maintenance projects, while ranchers have been able to graze cattle without the need of significant supplemental feed due to the lack of snow cover. For non-agricultural sectors of the Nebraska economy, the lack of snow has been a boon to city snow removal budgets and less energy demand used for winter heating by consumers.

Since the beginning of 2022, a strong upper air trough anchored over the Hudson Bay region has resulted in persistent cold across the western Great Lakes region. The Minnesota state climate office has indicated that at least 15 Alberta clipper systems have hit northern Minnesota since winter began. Here in Nebraska, these same systems pushed dry cold fronts through the state because of the lack of moisture, since these polar fronts moving southward originated out of northern Canada, far from any source of ocean water vapor.

There has been a subtle change to this pattern recently as two major winter storms have move across the southern High Plains region into the Ohio River valley. Although these two systems bypassed us to the south, they have provided beneficial surface moisture to the eastern half of Kansas, Oklahoma and Texas.

If this trend continues, low level moisture transported northward from the Gulf of Mexico in advance of storms ejecting out of the southern half of the Rocky Mountains will be more effective in generating precipitation across Nebraska. This is because vegetation south of Nebraska will be transpiring moisture into the boundary layer above soil surfaces and it will take less low level moisture advection from the Gulf of Mexico to enhance precipitation events as systems move across Nebraska.

Since the upper air trough influencing the Great Lakes region has persisted for nearly 7 weeks, the atmosphere is due to shift trough positions from the eastern to western United States. Long term ridge and trough patterns climatologically last around six weeks in length, but can vary from 4 to 8 weeks at a time. Therefore, based upon climatological averages, the atmosphere should move toward more storm activity moving eastward from the west coast, instead of moving from Canada southeastward toward the Great Lakes.

If La Nina conditions across the Equatorial Pacific continue to rapidly diminish, then the colder than normal sea surface temperature (SST) anomalies will give way to normal to above normal SST’s in the eastern half of the basin as the spring season progresses. Figure 3 shows the movement of sub-surface heat anomalies underneath the Equatorial Pacific. As you can see, the final surge of below normal temperature anomalies are coming to the surface. In addition, there are no below normal temperature anomalies below the surface all the way westward toward Indonesia and Australia.

As this subsurface warm pool reaches the eastern Equatorial Pacific surface, it will begin to spread westward with the trade winds and increase evaporation off of the western Mexico coastline. Therefore, any upper air lows working into the western United States will have a better connection to tropical moisture. This is especially important for any lows that move down the western U.S. coastline and form a cutoff low over the southwestern desert region. With additional moisture availability, these southwest lows should be able to survive moving east-northeast into the nation’s midsection, instead of dying a slow death from dry desert air cutting off its circulation pattern.

Additionally, March and April a critical time in regards to the Rocky Mountain snowpack. Approximately 40% of the water stored in this snowpack climatologically occurs during the next two months. In order for the central and southern Rocky snowpack to stay in the normal to above normal range, storm systems will need to move through the southern Great Basin before swinging northeast. If this fails to materialize, there is a high probability that CPC’s spring precipitation outlook will verify.

At present, it appears to me that the Hudson Bay upper air trough is beginning to break down, which would allow for more active weather to move from the Gulf of Alaska into the western United States. Therefore, I currently favor an active weather pattern developing across High Plains region over the next two months, which would be in opposition to CPC’s current Spring precipitation outlook.

Given the amount of cold air bottled up from western through eastern Canada, systems coming out of the western United States would have more than enough cold air being pulled into the backside of surface low pressure systems to create significant snow events like the southern Plains has experienced over the past two weeks. Thus, ranchers should be aware that the dry, open winter we have experienced will likely be more challenging entering calving season, if my assumptions come to fruition.

Al Dutcher, Agricultural Extension Climatologist, Nebraska State Climate Office

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