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Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD [email protected]...

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Dr. Sara Via, Professor, UMD [email protected] 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD, College Park [email protected] Source: NASA, Climate Central Difference from average temperatures 1881-1910 2016 the hottest year ever How do we know this is not part of a natural cycle? 320 340 360 380 300 180 200 220 240 260 280 2013 CO 2 concentration: 400 ppm 0 800,000 700,000 600,000 500,000 400,000 300,000 200,000 100,000 Age (years Before Present) Source: National Climatic Data Center, NOAA ~9 deg CO 2 Concentration Temperature Some energy is radiated back into space as infrared (heat) waves Some energy is radiated back into space as infrared (heat) waves Greenhouse gas molecules absorb infrared waves and reflect some heat back to Earth, slowing heat loss *more gas molecules, **slower heat loss ***more warming Greenhouse gas molecules absorb infrared waves and reflect some heat back to Earth, slowing heat loss *more gas molecules, **slower heat loss ***more warming Most solar radiation is absorbed by the Earth and warms it Most solar radiation is absorbed by the Earth and warms it More CO 2 in the atmosphere slows heat loss p.1
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Page 1: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

Managing Risk in a Changing Climate

Dr. Sara ViaDept. of Entomology & UME

UMD, College [email protected] Source: NASA, Climate Central

Difference from average temperatures 1881-1910

2016 the hottest year ever

400How do we know this is not part of a natural cycle?

320

340

360

380

300

180

200

220

240

260

280

2013 CO2 concentration: 400 ppm

0800,000 700,000 600,000 500,000 400,000 300,000 200,000 100,000

Age (years Before Present)Source: National Climatic Data Center, NOAA

~9 deg

CO

2 C

once

ntra

tion

Tem

pera

ture

Some energy is radiated back into space asinfrared (heat) waves

Some energy is radiated back into space asinfrared (heat) waves

Greenhouse gas molecules absorb infrared waves and reflect some heat back to Earth, slowing heat loss*more gas molecules, **slower heat loss***more warming

Greenhouse gas molecules absorb infrared waves and reflect some heat back to Earth, slowing heat loss*more gas molecules, **slower heat loss***more warming

Most solar radiation is absorbed by theEarth and warms it

Most solar radiation is absorbed by theEarth and warms it

More CO2 in the atmosphere slows heat loss

p.1

Page 2: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

-Warmer air-Warmer ocean-More water vapor in air-Higher sea levelThese cause- Severe weather; more extreme extremes- More variable weather- Warmer winters, earlier springs, hotter summers

- More rainfall comes as downpours; flash flooding- Rainy springs & falls (MD)- Dryer summers- More tidal flooding and storm surge

Useful to start planning NOW

The “New Normal”

2/8/2017

What does this look like for Maryland? Temperature

Source: NOAA

Average, maximum & minimum temperatureincrease in all seasons

1950 20145-year intervals

Annual Temperature

Days over 80 deg

Days over 100 deg

Nights over 70 deg

Nights over 80 deg

1950 2014 1950 2014

1950 2014 1950 2014

The New Normal in Maryland Growing Degree Days

30-year average

The New Normal in Maryland Growing Degree Days

2016

p.2

Page 3: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

- Northeast nights 4.4o warmer than in 1970- Fewer cold nights for required plant chilling

- perennials, bulbs, fruit trees (apples, peaches)

Effects of Climate Change: Temperature

Wolfe DW et al. 2005. Internat J Biometeor 49:303-309.]

Warmer winters = earlier bloomingNY apples bloom 8 days earlier than in the 1960s

Grapes bloom 6 days earlier

Late spring cold snap freezing, fruit lossPlant new orchards on hilltops, plant longer season varieties?

.

Effects of warmer winters, earlier springsPest insects

- better overwinter survival

- earlier appearance

- more generations/yr

- range expansion

- be vigilant & scout!!

- expect the unexpected

Mismatched timing in species interactions

Corn earworm in New Zealand

Species respond differently to warming– impacts biocontrol:- Host adds a generation,

but parasitoid doesn’t

Also affects plants and pollinators

Hysoppus pallidus, parasitoid of codling moth

p.3

Page 4: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

Insect controlInsectary plants attract beneficials,

increase their diversityProvide natural enemies nectar, pollen& protection from predators

Plant mixtures?

Bachelor buttons in celery, beneficials reduce aphids

Lacewing eggs

Heat stress: sun scald

ozone damage!

scald

Adapting to increased temperature- Plant earlier in spring, later in summer- Stagger planting dates to hedge bets- Mulch (plant material, white or reflective)- Try heat tolerant varieties- Build shade, evaporative cooling?

2104: Oakmoor Orchard, BC lost 40% Granny Smith yield to sun scald. Saved $47,000/yr with overhead evaporative cooling

http://www.sustainability.vic.gov.au/services-and-advice/business/energy-and-materials-efficiency-for-business/case-studies/agriculture-case-studies/oakmoor-orchards

Precipitation: 5” more/year than in 1900

p.4

Page 5: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

What does this look like for Maryland?Rainfall

Source: NOAA

Observed rainfall inSpring Summer Fall

1950 20145-year intervals

Observed number of rains > 4”

1950 2014 1950 2014 1950 2014May delay planting, wash out or contaminate fields,

stunt or kill plants, increase disease, cause soil compaction, risk of hail

-Improve drainage

- Improve soil health forbetter infiltration

- Prevent erosion/ cover crops- Use flood-resistant rootstocks- Stagger planting dates- Diversify crops

Spring/Fall flooding: adaptation strategies

Beware: Floods can compromise food safety

Summer drought: adaptation strategies

- Add irrigation (if water available)increase water storage?

- Build up the soil- more organicmatter holds water

- Add mulch?

- Grow cover crops betweenrows and mulch?

- Fruit trees need water mostearly in season, late summerdrought not a problem?

p.5

Page 6: Dr. Sara Via - University of Maryland Extension...Dr. Sara Via, Professor, UMD svia@umd.edu 2/16/2017 Managing Risk in a Changing Climate Dr. Sara Via Dept. of Entomology & UME UMD,

Dr. Sara Via, Professor, UMD [email protected] 2/16/2017

Drip Irrigation for Fruits &Vegetables Irrigation: Use water wisely

Use online tool to time irrigation:Cornell Climate-Smart Farming

Water Deficit Calculator

Useful Resources for Climate-Smart Farming

Would you like to work on an adaptation plan for your farm?Interested?? Leave your email on the sign-up sheet

p. 6


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