how does this balance between insolation and outgoing longwave radiation manifest itself globally?

26

HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY? Meridional Radiation Balance and Transfer

Upload: taylor

Post on 22-Feb-2016

56 views

Category:

Documents

0 download

Report

Download

Tags:

Embed Size (px):

DESCRIPTION

HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?. Meridional Radiation Balance and Transfer. Annual Radiation. 0°. 90°. Latitude. Insolation. Annual Radiation. Insolation. 0°. 90°. Latitude. Insolation. Outgoing. Outgoing. - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Meridional Radiation Balance and Transfer

Page 2: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

0° 90°Latitude

Annu

al R

adia

tion

Page 3: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

0° 90°Latitude

Annu

al R

adia

tion

Page 4: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

0° 90°Latitude

Annu

al R

adia

tion

Page 5: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

0° 90°Latitude

Surplus

Annu

al R

adia

tion

Page 6: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

0° 90°Latitude

Deficit

Surplus

Annu

al R

adia

tion

Page 7: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°Latitude

Deficit

Surplus

Annu

al R

adia

tion

Insolation = OutgoingBalance equals zero

Page 8: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°Latitude

Deficit

Surplus

Annu

al R

adia

tion

Page 9: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°Latitude

Deficit

Surplus

Annu

al R

adia

tion

Page 10: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

What can you see?

Annual differences in Incoming and outgoing radiation at top of the atmosphere.

Page 11: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

Annu

al R

adia

tion

Page 12: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Page 13: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Energy Transfer as Freight Train

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Page 14: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 15: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 16: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 17: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 18: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 19: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 20: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 21: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 22: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 23: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 24: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Page 25: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Maximum PolewardEnergy Transfer

Page 26: HOW DOES THIS BALANCE BETWEEN INSOLATION AND OUTGOING LONGWAVE RADIATION MANIFEST ITSELF GLOBALLY?

Insolation

Insolation

OutgoingOutgoing

~35°0° 90°

Transfer

Latitude

Deficit

Surplus

50% Surface Area 50% Surface Area

Annu

al R

adia

tion

Annu

al P

olew

ard

Tran

sfer

Poleward Energy Transfer

TOPIC 6: INSOLATIO N AND THE SEASONS. Solar Radiation and Insolation Insolation – Incoming solar radiation Components of Insolation (by EM type) → Infrared

Results of Outgoing Longwave Radiation and Albedo over

FILL-IN NOTES. Insolation = INcoming SOLar RadiATION (sunlight) Angle of Insolation: Angle of the sun above the horizon Duration of Insolation:

November 2019 Geography Higher level and standard level ... PAST PAPERS...Longwave/outgoing radiation [1] is absorbed by greenhouse gases [1], heating up the atmosphere [1]. (b) Explain

Soil Temperature. Energy balance Incoming shortwave from sun Incoming shortwave from sun Outgoing longwave from earth-atmosphere Outgoing longwave from

METR 415/715 Monday March 11 2013. Outgoing Longwave Radiation at top of atmosphere Broadband IR radiation The PSD Map Room The utility and limitations

TOA Outgoing Clear-Sky Longwave Radiation (rlutcs)...2012/06/06 · Figs. 1a and 1b provide regional plots of mean clear-sky LW TOA flux and interannual variability for the month

Solar Radiation and Insolation

ScaRaB on Megha-Tropiques - NASA · 2011. 11. 22. · ScaRaB goal : To determine the longwave and shortwave outgoing ﬂuxes observaons at the TOA. L LW (daytime)=L TOTAL – A’×L

Technical Note on CERES EBAF Ed2.7 TOA Outgoing Longwave

Relationships between outgoing longwave radiation and ... · Relationships between outgoing longwave radiation and diabatic heating in reanalyses 1 3 Fig. 1 Example time series at

12 temperature, emr, insolation

T°CT°C et Salinité. Figure 5.7 Upper: Zonal averages of heat transfer to the ocean by insolation QSW, and loss by longwave radiation QLW, sensible heat

Climate Data Record (CDR) Program · 2017. 3. 1. · CDR Program Outgoing Longwave Radiation - Monthly CDRP-ATBD-0097 Rev. 3 01/08/2014 Page 8 2.2 Instrument Characteristics HIRS

The ThreeThe Three--Dimensional CirculationDimensional ...4. Run General Circulation Model to Obtain next First Guess 5 6 Mean January Outgoing Longwave Radiation (OLR), 1979-2001

Identifying How Outgoing Longwave Radiation Patterns

6 i-longwave radiation

Estimating the outgoing longwave radiation from the FY-3B ... · OLR, infrared radiation transfer, inverse model, regression analysis, validation Citation: Wu X, Yan J J. Estimating

TOA Outgoing Clear-Sky Longwave Radiation (rlutcs)

ELNINO AND OUTGOING LONGWAVE RADIATION · flux atthe so-called"top of the atmosphere." This parameter, during production, is binned regional variations in the diurnal cycle in the

The Spectral Dimension of Arctic Outgoing Longwave ... · The Spectral Dimension of Arctic Outgoing Longwave Radiation and Greenhouse Efficiency Trends from 2003 to 2016 Colten Peterson

Tropical cyclone influence on the long-term variability of ... · 2002) used satellite data of outgoing longwave radiation (OLR) to define an index of convective activity. Kubota

Topic 6 Insolation and the Seasons. Insolation (INcoming SOLar radiATION) Intensity of Insolation depends on the angle of the Sun’s rays, which are due

Longwave Receiver

Mechanisms for climate variability ... - empslocal.ex.ac.ukempslocal.ex.ac.uk/people/staff/gv219/papers/loving-vallis-paleo05.pdf · the balance among insolation (S 0(1 # a )), outgoing

Modeling the change in spectrally resolved outgoing longwave radiation

Estimation of Outgoing Longwave Radiation from AIRS Radiance … · 2018. 7. 17. · Estimation of Outgoing Longwave Radiation from AIRS Radiance Observations Fengying Sun, Mitchell

Global Warming (Climate Change). Outline of Lectures Earth’s Energy Balance –incident solar energy –outgoing longwave radiation –detailed energy balance

Angle of insolation

Insolation Insolation = Incoming Solar Radiation Energy in = Energy out or, Insolation In = Heat Out (Earth only emits heat)

Development of IASI Outgoing Longwave Radiation Algorithm · 2015. 4. 24. · Ellingson, R. G., D. J. Yanuk, H.-T. Lee and A. Gruber, 1989: A technique for estimating outgoing longwave

Coupled versus Uncoupled hindcast simulations of the MJO in ......Lag correlations between Outgoing Longwave Radiation (OLR) and SST anomalies are calculated, to determine the relationship

NUCAPS Outgoing Longwave Radiation Algorithm Theoretical ...AVHRR Advanced Very High Resolution Radiometer CERES The Cloud and the Earth’s Radiant Energy System ... 12 µm) from

HIRS Outgoing Longwave Radiation—Daily Climate Data Record ...€¦ · HIRS also has more spectral channels, including those for measuring water vapor, which provides a more accurate

NOAA Unique CrIS ATMS Processing System (NUCAPS) · Vertical CO Profile Vertical CO. 2. Profile Vertical CH. 4. Profile Outgoing Longwave Radiation (OLR) Vertical HNO. 3. Profile