turn north of the warm front south of the warm front warm ...mia. prepare for and be aware of...

1
National Oceanic and Atmospheric Administration NOAA - https://www.noaa.gov NOAA Education Portal - https://www.noaa.gov/education National Weather Service NWS Education - https://www.weather.gov/owlie JetStream - An Online School for Weather - https://www.weather.gov/jetstream NOAA Weatherwise Warm front Warmer air replacing cool (or cold) air Cold front Cold (or cooler) air replacing warmer air Dry line Boundary dividing dry desert air from moist gulf air H High pressure Location of highest surface air pressure Stationary front Non-moving boundary dividing warm air from cooler air Surface wind Jet stream L Low pressure Location of lowest surface air pressure iding air H High pressure Location of highest surface Surface wind Jet L Low pressure Location of lowest surface H H L H H H H L L L L L H H L J e t s t r e a m Equator Polar jet stream Subtropical jet stream Tropical air Temperate air Polar air Strong winds from the high-pressure system carry colder, drier air into the dark blue area. As the cold front passes, precipitation ends and skies clear fairly rapidly. Possible impacts The difference in air pressure between two points determines wind speed and direction. Large pressure differences cause very strong winds. They are more likely to occur in winter and can lead to blizzard conditions and dangerous wind chills. In mountainous areas, lightning from thunderstorms with little or no rainfall can ignite wildfires. These fires may spread rapidly when driven by strong winds associated with the thunderstorm. Weather safety Remember: Ice and Snow, Take It Slow! both on and off the road. While driving, slow down to reduce the chance of an accident on slippery roads. Don’t overexert yourself when shoveling. Avoid prolonged exposure to cold temperatures, which can cause frostbite and/or hypothermia. Prepare for and be aware of potential fire hazards during dry periods. North of the cold front In the light blue area, the air tends to be cool and dry. Closer to the warm front, moisture increases. As a result, clouds thicken, which can lead to rain or snow. Possible impacts Warm fronts near areas of low-pressure can bring heavy rain, snow, or sleet. Rain can lead to flooding, while snow and sleet may result in a variety of hazards including slick roads and power outages. Weather safety Never drive into flooded roadways or around a barricade. Turn Around Don’t Drown! Know the risks of floods and plan your evacuation route. Have extra food and water in case you lose power or are trapped in your home. During winter weather, drive slowly or not at all. North of the warm front Warm, moist air from the Gulf of Mexico and Atlantic Ocean moves into the green area, increasing temperatures and humidity. Showers and thunderstorms can develop along and in advance of a cold front or dry line. Possible impacts Warm, moist air can be forced upwards as it reaches an approaching cold front and/or dry line. This can cause severe thunderstorms, flooding, and tornadoes. Weather safety Always be Weather-Ready — forecasts can provide several days advance notice of storms. Check them regularly. Be prepared and When Thunder Roars, Go Indoors to stay safe from lightning. Know your safe place at home and work. South of the warm front South of the fronts and west of the dry line In the orange area, weather is generally dry and mild. Approaching fronts can lead to high altitude thunderstorms over mountain peaks, resulting in strong winds at the surface. Over time the effects of the fronts will diminish. To learn more about the characteristics of fronts, explore the rest of the map. Possible impacts Strong surface winds can lead to dust storms and wildfires. In Southern California, the warm, dry Santa Ana winds blow towards the coast from the high desert areas. Seasonal heavy rain, even from distant thunderstorms, can lead to flash floods and debris flows in typically very dry areas. Weather safety Be alert for dust storms, which can come with little warning — Pull Aside, Stay Alive. Pull far off the road and turn all car lights off. Follow evacuation orders during fires. Monitor forecasts for flash floods, which can be a risk many miles from a storm, especially in dry valleys and canyons. Don’t be caught off guard; be prepared to move to higher ground. Explore more weather phenomena at www.weather.gov/jetstream Drawing Conclusions • Toasty Wind A Pressing Engagement • Going with the Flow Suggested lessons: he weather we experience every day on the ground is a result of what is happening far above our heads. Up there, the air is always moving as heat energy is redistributed across the Earth. Meteorologists study air movement to make weather forecasts. The Sun heats the Earth, which then heats the air in the atmosphere. Because the Sun hits the equator most directly, the air at the equator receives more heat energy than the air closer to the poles. This warm air rises because it is less dense than cool air. When the warm air reaches the upper atmosphere, it can no longer rise and is forced toward the poles. As the air cools, it becomes denser and falls back toward Earth. High-pressure areas form where cooler air is falling towards the Earth. Low-pressure areas form where warm air is rising. Air circulates from areas of high pressure to areas of low pressure. The way the air moves affects the weather. Between the large areas of circulating air, jet streams form. Jet streams are tube-like paths of strong wind moving from West to East around the globe. The position and strength of jet streams vary from North to South, as well as vertically throughout the atmosphere. The location of the jet streams and their seasonal movement drive major weather patterns around the world. In the United States, cold snaps happen when the polar jet stream dips south. Heat waves can occur when the polar jet stream is very far north, allowing for warm sub-tropical air to move north. T Be weatherwise wherever you are This map shows a simplified forecast for a single, hypothetical day. The locations of the low- and high-pressure systems, jet stream, and fronts shape the weather that a given region may experience. There can be hazardous weather anywhere, at any time. Begin each day knowing the weather forecast. If severe or extreme weather is a possibility, periodically check for forecast updates. Be prepared with a safety plan. Have a “go-kit” with important property and documents ready in case of emergency. Have at least a three-day supply of food and water. Learn the specific recommendations for regional and seasonal weather hazards. Learn more about seasonal safety at https://www.weather.gov/safetycampaign. C M Y CM MY CY CMY K cloudchart_back_082919.ai 1 8/29/2019 10:57:14 AM cloudchart_back_082919.ai 1 8/29/2019 10:57:14 AM

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Page 1: Turn North of the warm front South of the warm front Warm ...mia. Prepare for and be aware of potential fire hazards during dry periods. North of the cold front In the light blue area,

Nat

iona

l Oce

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and

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Adm

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tratio

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OAA

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Edu

catio

n Po

rtal -

http

s://w

ww.

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.gov

/edu

catio

n

Nat

iona

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ther

Ser

vice

NW

S Ed

ucat

ion

- http

s://w

ww.

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ther

.gov

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lieJe

tStre

am -

An O

nlin

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hool

for W

eath

er -

http

s://w

ww.

wea

ther

.gov

/jets

tream

NO

AA

Wea

ther

wis

e

War

m fr

ont

War

mer

air

repl

acin

g co

ol (o

r col

d) a

ir

Col

d fro

ntC

old

(or c

oole

r)ai

r rep

laci

ng

war

mer

air

Dry

line

Boun

dary

div

idin

gdr

y de

sert

air

from

moi

st

gulf

air

HHi

gh p

ress

ure

Loca

tion

of

high

est s

urfa

ceai

r pre

ssur

e

Stat

iona

ry fr

ont

Non

-mov

ing

boun

dary

divi

ding

war

m

air f

rom

coo

ler a

ir

Surfa

ce w

ind

Jet

stre

am

LLo

w p

ress

ure

Loca

tion

of

low

est s

urfa

ce

air p

ress

ure

idin

gai

r

HHi

ghpr

essu

reLo

catio

n of

hi

ghes

tsur

face

Surfa

ce w

ind

Jet

LLo

wpr

essu

reLo

catio

n of

lo

wes

tsur

face

HH

LHHHH

LLLLLHH

L

Jet s

tre

am

Equa

tor

Pola

r jet

str

eam Su

btro

pica

l je

t str

eam

Trop

ical

air

Tem

pera

teai

r

Pola

r air

Stro

ng w

inds

from

the

high

-pre

ssur

e sy

stem

car

ry c

olde

r, dr

ier a

ir in

to th

e da

rk b

lue

area

. As

the

cold

fron

t pa

sses

, pre

cipi

tatio

n en

ds a

nd s

kies

cle

ar fa

irly

rapi

dly.

Poss

ible

impa

cts

The

diffe

renc

e in

air

pres

sure

bet

wee

n tw

o po

ints

det

erm

ines

win

d sp

eed

and

dire

ctio

n. L

arge

pre

ssur

e di

ffere

nces

cau

se v

ery

stro

ng w

inds

. The

y ar

e m

ore

likel

y to

occ

ur in

win

ter a

nd c

an le

ad to

bliz

zard

con

ditio

ns

and

dang

erou

s w

ind

chills

. In

mou

ntai

nous

are

as, l

ight

ning

from

thun

ders

torm

s w

ith li

ttle

or n

o ra

infa

ll ca

n ig

nite

wild

fires

. The

se fi

res

may

spr

ead

rapi

dly

whe

n dr

iven

by

stro

ng w

inds

ass

ocia

ted

with

the

thun

ders

torm

.

Wea

ther

saf

ety

Rem

embe

r: Ic

e an

d Sn

ow, T

ake

It Sl

ow! b

oth

on a

nd o

ff th

e ro

ad. W

hile

driv

ing,

slo

w d

own

to re

duce

the

chan

ce o

f an

acci

dent

on

slip

pery

road

s. D

on’t

over

exer

t you

rsel

f whe

n sh

ovel

ing.

Avo

id p

rolo

nged

exp

osur

e to

col

d te

mpe

ratu

res,

whi

ch c

an c

ause

fros

tbite

and

/or h

ypot

herm

ia. P

repa

re fo

r and

be

awar

e of

pot

entia

l fire

ha

zard

s du

ring

dry

perio

ds.

Nor

th o

f the

col

d fr

ont

In th

e lig

ht b

lue

area

, the

air

tend

s to

be

cool

and

dry

. Clo

ser t

o th

e w

arm

fron

t, m

oist

ure

incr

ease

s. A

s a

resu

lt, c

loud

s th

icke

n,

whi

ch c

an le

ad to

rain

or s

now.

Poss

ible

impa

cts

War

m fr

onts

nea

r are

as o

f low

-pre

ssur

e ca

n br

ing

heav

y ra

in,

snow

, or s

leet

. Rai

n ca

n le

ad to

floo

ding

, whi

le s

now

and

sle

et

may

resu

lt in

a v

arie

ty o

f haz

ards

incl

udin

g sl

ick

road

s an

d po

wer

out

ages

.

Wea

ther

saf

ety

Nev

er d

rive

into

floo

ded

road

way

s or

aro

und

a ba

rrica

de. T

urn

Aro

und

Don

’t D

row

n! K

now

the

risks

of f

lood

s an

d pl

an y

our

evac

uatio

n ro

ute.

Hav

e ex

tra fo

od a

nd w

ater

in c

ase

you

lose

po

wer

or a

re tr

appe

d in

you

r hom

e. D

urin

g w

inte

r wea

ther

, driv

e sl

owly

or n

ot a

t all.

Nor

th o

f the

war

m fr

ont

War

m, m

oist

air

from

the

Gul

f of M

exic

o an

d At

lant

ic O

cean

mov

es in

to th

e gr

een

area

, in

crea

sing

tem

pera

ture

s an

d hu

mid

ity. S

how

ers

and

thun

ders

torm

s ca

n de

velo

p al

ong

and

in

adva

nce

of a

col

d fro

nt o

r dry

line

.

Poss

ible

impa

cts

War

m, m

oist

air

can

be fo

rced

upw

ards

as

it re

ache

s an

app

roac

hing

col

d fro

nt a

nd/o

r dry

line

. Th

is c

an c

ause

sev

ere

thun

ders

torm

s, fl

oodi

ng,

and

torn

adoe

s.

Wea

ther

saf

ety

Alw

ays

be W

eath

er-R

eady

— fo

reca

sts

can

prov

ide

seve

ral d

ays

adva

nce

notic

e of

sto

rms.

C

heck

them

regu

larly

. Be

prep

ared

and

W

hen

Thun

der R

oars

, Go

Indo

ors

to s

tay

safe

fro

m li

ghtn

ing.

Kno

w y

our s

afe

plac

e at

hom

e an

d w

ork.

Sou

th o

f the

war

m fr

ont

Sout

h of

the

fron

ts a

nd

wes

t of t

he d

ry li

neIn

the

oran

ge a

rea,

wea

ther

is g

ener

ally

dry

an

d m

ild. A

ppro

achi

ng fr

onts

can

lead

to h

igh

altit

ude

thun

ders

torm

s ov

er m

ount

ain

peak

s,

resu

lting

in s

trong

win

ds a

t the

sur

face

. Ove

r tim

e th

e ef

fect

s of

the

front

s w

ill di

min

ish.

To le

arn

mor

e ab

out t

he c

hara

cter

istic

s of

fron

ts,

expl

ore

the

rest

of t

he m

ap.

Poss

ible

impa

cts

Stro

ng s

urfa

ce w

inds

can

lead

to d

ust s

torm

s an

d w

ildfir

es. I

n So

uthe

rn C

alifo

rnia

, the

war

m,

dry

Sant

a An

a w

inds

blo

w to

war

ds th

e co

ast

from

the

high

des

ert a

reas

. Sea

sona

l hea

vy

rain

, eve

n fro

m d

ista

nt th

unde

rsto

rms,

can

lead

to

flas

h flo

ods

and

debr

is fl

ows

in ty

pica

lly v

ery

dry

area

s.

Wea

ther

saf

ety

Be a

lert

for d

ust s

torm

s, w

hich

can

com

e w

ith

little

war

ning

— P

ull A

side

, Sta

y A

live.

Pul

l far

of

f the

road

and

turn

all

car l

ight

s of

f. Fo

llow

ev

acua

tion

orde

rs d

urin

g fir

es. M

onito

r fo

reca

sts

for f

lash

floo

ds, w

hich

can

be

a ris

k m

any

mile

s fro

m a

sto

rm, e

spec

ially

in d

ry

valle

ys a

nd c

anyo

ns. D

on’t

be c

augh

t off

guar

d;

be p

repa

red

to m

ove

to h

ighe

r gro

und.

Expl

ore

mor

e w

eath

er p

heno

men

a at

ww

w.w

eath

er.g

ov/je

tstr

eam

Dra

win

g C

oncl

usio

ns •

Toas

ty W

ind

A Pr

essi

ng E

ngag

emen

t • G

oing

with

the

Flow

Sugg

este

d le

sson

s:

he w

eath

er w

e ex

perie

nce

ever

y da

y on

the

grou

nd is

a re

sult

of w

hat i

s ha

ppen

ing

far a

bove

our

hea

ds. U

p th

ere,

the

air i

s al

way

s m

ovin

g as

hea

t ene

rgy

is re

dist

ribut

ed a

cros

s th

e Ea

rth.

Met

eoro

logi

sts

stud

y ai

r mov

emen

t to

mak

e w

eath

er fo

reca

sts.

The

Sun

heat

s th

e Ea

rth, w

hich

then

hea

ts th

e ai

r in

the

atm

osph

ere.

Bec

ause

the

Sun

hits

the

equa

tor

mos

t dire

ctly,

the

air a

t the

equ

ator

rece

ives

mor

e he

at e

nerg

y th

an th

e ai

r clo

ser t

o th

e po

les.

Thi

s w

arm

air r

ises

bec

ause

it is

less

den

se th

an c

ool a

ir.

Whe

n th

e w

arm

air

reac

hes

the

uppe

r atm

osph

ere,

it c

an n

o lo

nger

rise

and

is fo

rced

tow

ard

the

pole

s.

As th

e ai

r coo

ls, i

t bec

omes

den

ser a

nd fa

lls b

ack

tow

ard

Earth

. Hig

h-pr

essu

re a

reas

form

whe

re c

oole

r

air i

s fa

lling

tow

ards

the

Earth

. Low

-pre

ssur

e ar

eas

form

whe

re w

arm

air

is ri

sing

. Air

circ

ulat

es fr

om

area

s of

hig

h pr

essu

re to

are

as o

f low

pre

ssur

e.

The

way

the

air m

oves

affe

cts

the

wea

ther

. Bet

wee

n th

e la

rge

area

s of

circ

ulat

ing

air,

jet s

trea

ms

form

.

Jet s

tream

s ar

e tu

be-li

ke p

aths

of s

trong

win

d m

ovin

g fro

m W

est t

o Ea

st a

roun

d th

e gl

obe.

The

pos

ition

and

stre

ngth

of j

et s

tream

s va

ry fr

om N

orth

to S

outh

, as

wel

l as

verti

cally

thro

ugho

ut th

e at

mos

pher

e.

The

loca

tion

of th

e je

t stre

ams

and

thei

r sea

sona

l mov

emen

t driv

e m

ajor

wea

ther

pat

tern

s ar

ound

the

wor

ld. I

n th

e U

nite

d St

ates

, col

d sn

aps

happ

en w

hen

the

pola

r jet

stre

am d

ips

sout

h. H

eat w

aves

can

occu

r whe

n th

e po

lar j

et s

tream

is v

ery

far n

orth

, allo

win

g fo

r war

m s

ub-tr

opic

al a

ir to

mov

e no

rth.

TBe

wea

ther

wis

e w

here

ver y

ou a

reTh

is m

ap s

how

s a

sim

plifi

ed fo

reca

st fo

r a s

ingl

e, h

ypot

hetic

al d

ay.

The

loca

tions

of t

he lo

w- a

nd h

igh-

pres

sure

sys

tem

s, je

t stre

am,

and

front

s sh

ape

the

wea

ther

that

a g

iven

regi

on m

ay e

xper

ienc

e.

Ther

e ca

n be

haz

ardo

us w

eath

er a

nyw

here

, at a

ny ti

me.

Beg

in

each

day

kno

win

g th

e w

eath

er fo

reca

st. I

f sev

ere

or e

xtre

me

wea

ther

is a

pos

sibi

lity,

per

iodi

cally

che

ck fo

r for

ecas

t upd

ates

. Be

pre

pare

d w

ith a

saf

ety

plan

. Hav

e a

“go-

kit”

with

impo

rtant

pr

oper

ty a

nd d

ocum

ents

read

y in

cas

e of

em

erge

ncy.

Hav

e at

leas

t a

thre

e-da

y su

pply

of f

ood

and

wat

er. L

earn

the

spec

ific

reco

mm

enda

tions

for r

egio

nal a

nd s

easo

nal w

eath

er h

azar

ds.

Lear

n m

ore

abou

t sea

sona

l saf

ety

at

http

s://w

ww.

wea

ther

.gov

/saf

etyc

ampa

ign.

C M Y CM MY

CY CMY

K

clou

dcha

rt_b

ack_

0829

19.a

i 1

8/

29/2

019

10:

57:1

4 A

Mcl

oudc

hart

_bac

k_08

2919

.ai

1

8/29

/201

9 1

0:57

:14

AM