Predicting Growing Season Grassland Production in the Spring using Sea Surface Temperatures, NDVI, and Grass-Cast

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Predicting Growing Season Grassland Production in the Spring using Sea Surface Temperatures, NDVI, and Grass-Cast William Parton 1, Melannie Hartman 1, Maosi Chen 1, Stephen Del Grosso 1,2, Justin Derner 2, Brian Fuchs 3, Alan Knapp 4, Darin Schulte 5, Bill Smith 6 1 Natural Resource Ecology Laboratory, Colorado State University 2 U.S. Department of Agriculture, Agricultural Research Services 3 University of Nebraska, Lincoln 4 Warner College of Natural Resources, Colorado State University 5 North Central Climate Center, Fort Collins, CO 6 University of Arizona

Outline Correlation of annual aboveground plant production (ANPP) to Rainfall Variables and AVHRR NDVI data (1982 to 2014) Long term annual ANPP data from Cheyenne (1940 to 2014) Site-level AVHRR NDVI and ANPP Regional Great Plains simulated AET using the DayCent ecosystem model Using Grass-Cast to simulate seasonal forecast of ANPP for the Great Plains Conclusions

Cheyenne Correlation of ANPP to Rainfall Variables Site Apr May Apr Jun Apr Jul Apr Aug Apr Sep Annual Cheyenne Precipitation 0.4053 0.5685 0.5966 0.361 0.2003 0.2111 Transpiration 0.0648 0.3428 0.5838 0.4882 0.4612 0.4609 AET 0.2275 0.4527 0.6478 0.5152 0.4711 0.4082

Correlation of April to July Cumulative Actual Evapotranspiration (iaet) to Grassland Plant production (ANPP)

Site-level AVHRR NDVI vs. ANPP (1982-2016)

Difference in R 2 when AET (April-July) is correlated to cumulative (May-September) NDVI vs when Precipitation (April-July) is correlated to cumulative NDVI

Actual Evapotranspiration (CPER, 2003) No text Volumetric Soil Water Content (CPER, 2003) Actual Evapotranspiration (Konza, 2009)

Grass-Cast Project Goals Predict total growing season above-ground grassland plant production (ANPP) for all Great Plains counties in the Spring as function of the April to July cumulative actual evapotranspiration water loss (iaet) Starting in April, update ANPP forecasts every two weeks based on current weather data and new precipitation forecasts (monthly basis).

Forecast Procedure 1. Use DayCent model to simulate 2018 county-level iaet (36 model runs per county) where the remainder of 2018 is replaced by analog weather data that was observed from 1982-2017. Weather is ranked by May-July precipitation. 2. For each model run, make prediction of growing season cumulative NDVI (indvi) based on county-level correlation of iaet to indvi. 3. For each indvi prediction, use the Great Plains correlation of indvi to ANPP to predict annual ANPP for each county. 4. Three forecasts: below-normal, normal, and above normal MJJ precipitation using the results from the 12 driest, 12 moderate, and 12 wettest years from 1982-2017.

Grass-Cast 2017 Growing Season ANPP Forecasts (Percent change compared to 30-yr mean predicted ANPP) May 22 June 12 June 30

2002 (Dry Year) Actual NDVI compared to Predicted ANPP Percent change compared to 1982-2011 means 78% accurate NDVI ANPP

2009 (Wet Year) Actual NDVI compared to Predicted ANPP Percent change compared to 1982-2011 means 76% accurate NDVI ANPP

GrassCast ANPP forecasts for April 22, 2018

GrassCast ANPP forecasts for May 1, 2018

GrassCast ANPP forecasts for May 8, 2018

Conclusions ANPP in the Great Plains is correlated to AMO, PDO and ENSO sea surface temperature anomalies Plant productivity is correlated to NDVI. Both NDVI and NPP are correlated to AET. Grass-Cast has the potential to predict regional patterns of ANPP for the Great Plains given the observed weather data and seasonal forecasts of precipitation ANPP forecasts greatly improve after May 15 Grass-Cast forecast of ANPP are very similar to growing season observed NDVI data sets

Use of April Sea Surface Temperature (SST) anomalies to predict iaet for the Great Plains PDO and ENSO both negative PDO and ENSO both positive PDO/ENSO extremes PDO/ENSO -/- Driest Conditions for the Southern Great Plains PDO/ENSO +/+ Wettest Conditions for the Southern Great Plains PDO = Pacific Decadal Oscillation ENSO = El Niño Southern Oscillation

Use of April Sea Surface Temperature (SST) anomalies to predict iaet for the Great Plains PDO and AMO both negative PDO and AMO both positive PDO/AMO extremes PDO = Pacific Decadal Oscillation AMO = Atlantic Multidecadal Oscillation

Spring NDVI (May 4-12) correlates to growing season production (NDVI can be measured by drones as well as satellites) Zero Low Medium High