With the challenges of the drought, the beef cow inventory declined 3.1 percent for an annual inventory of 2011 and prospects for further decline are evident unless changes occur in cow slaughter and heifer retention. With this decline, the 2012 U.S. calf crop stands at 35 million head, the lowest in 60 years.
Updated February 2018 Droughts can have negative impacts on our pastures that could last for years to come. In addition, the more your pastures are stressed and overgrazed, the longer it will take...
Most producers are trying to survive the winter by stretching forage and feed resources. This can be accomplished with careful thought and consultation with a nutritionist to ensure that each cow's nutrient requirements are still being met for the stage of production it is in. If corners are cut to save money now, it can have long lasting repercussions.
Even with the rains during the fall of 2011, much of Oklahoma and Texas is still under drought advisories. Long-term forecasts are not promising for abundant rainfall during the spring or summer of 2012.
The likelihood of wildfires occurring increases during late fall and winter months due to dormant grass, fallen tree leaves and periods of high winds and low humidities.
The drought of 2011 will not soon be forgotten. It's been a year of record low rainfall and record high temperatures.
The Noble Research Institute offers assistance, continues research for drought-stricken Southern Great Plains.
As we manage the cow herd into the fall and through the winter, our primary focus should be on health and nutrition. These two areas of management determine reproductive performance, which is the number one factor that affects profitability.
As if to add insult to injury, drought conditions make weed control even more challenging and important than usual. Weeds compete for light, nutrients, space and, most importantly during a drought, water.
During times of drought, water quantity is an obvious concern to livestock producers. Livestock consume water daily, but evaporation is the primary means of water loss from earthen impoundments.