“Northern New England Climate: Past, Present, and...

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Weather instantaneous or synoptic measurements Climate time / space average Basic Concepts “Northern New England Climate: Past, Present, and Future”

Transcript of “Northern New England Climate: Past, Present, and...

Page 1: “Northern New England Climate: Past, Present, and Future”iceage.umeqs.maine.edu/ers121/2016/26_20th_century_warming.pdf · “Northern New England Climate: Past, Present, and

Weather instantaneous or synoptic measurements

Climate time / space average

Basic Concepts

“Northern New England Climate: Past, Present, and Future”

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Weather - the state of the air and atmosphere at a particular time and place : the temperature and other outside conditions (such as rain, cloudiness, etc.) at a particular time and place

temperature (average energy, ˚C) humidity (water vapor, g/kg) pressure (force/area, mb = 100 N/m2) winds (circulation, m/s) cloud cover (liquid/solid water) precipitation rate (mm/day)

Measurements of the following variables are used to quantify weather

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Climate is often defined as ‘average weather’, usually described in terms of the mean and variability of temperature, precipitation and wind over a period of time (typically 30 years).

Climate is also characterized by the frequency and magnitude of extreme weather events

A Definition of Climate

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hourly (synoptic)

daily mean daily range (diurnal cycle) monthly mean annual mean annual range (seasonal cycle)

air temperature data

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The average, or mean, of a meteorological variable is:Climate defined

And, the variance (a measure of how far a set of numbers is spread out:

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average daily temperature

30-year annual average = 51.7˚F

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average daily temperature

30-year annual average = 51.7˚F

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average daily temperature

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average monthly temperature

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internal dynamics example -

persistent ridging over western North

America

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internal dynamics example - persistent ridging over western North America

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average monthly temperature

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external forcing example - Mt. Pinatubo

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What Factors Are Involved In Changing Earth’s Climate?

Examples of external forcing include: solar variations volcanic eruptions changes in atmospheric composition

The climate system evolves over time under the influence of its own internal dynamics and due to changes in external forcing.

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IPCC, FAQ 1.3, Figure 1

✦ by changing the amount of incoming solar radiation

✦ by changing the fraction of solar radiation that is reflected back to space

✦ by altering the longwave radiation from Earth back towards space

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Radiative forcing of global climate

IPCC, FAQ 2.1, Figures 1 & 2

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Greenhouse gases increase dramatically since industrial revolution

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IPCC, FAQ 2.1, Figure 1

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Long-term record of globally averaged annual temperature

+1.2˚F/century

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Long-term record of annual average temperature for Massachusetts

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Long-term record of annual average precipitation for Massachusetts

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Long-term record of annual average temperature for Vermont

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Long-term record of annual average precipitation for Vermont

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Long-term record of annual average temperature for Maine

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Long-term record of annual average precipitation for Maine

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Lake ice-out

dates

Average ice-out dates for lakes in Maine come about two weeks earlier than they did in the late 19th century

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The length of the growing season in Maine has increased over the last 150 years

-40 to -30ºF -30 to -20ºF -20 to -10ºF -10 to 0ºF 0 to 10ºF

Plant hardiness zones have shifted northward over the past few decades

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River flow

Over the past 50 years flow has tended to increase in early spring and decrease in late spring/early summer

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Model projections of globally averaged surface temperature for

three emissions scenarios

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NCAR climate model

Future climate (21st century)

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✦ it has changed ✦ we see the impacts ✦ some of the change thus far is attributable

to human activity ✦ northern New England, like the rest of the

planet will experience significantly more change in the future

✦ the change impacts things that we care about

✦ we would like to predict future climate change

Observational Record of Global and Regional Climate: Key Facts

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Summary ✦ Greenhouse gas warming is evident

across northern New England

✦ It will continue, at an accelerated rate

✦ Precipitation across the state is likely to increase, less snow, more rain

✦ Climate will be more variable

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Questions?