aerial rivers and lake, subtropical rainfall and soil evaporation josefina moraes arraut, c. nobre,...

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Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General Assembly, April 5 2011

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Page 1: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Aerial Rivers and Lake, Subtropical Rainfall and

soil EvaporationJosefina Moraes Arraut,

C. Nobre, H.M.J. Barbosa, A. Marengo,

CCST - INPEEGU General Assembly, April 5

2011

Page 2: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Moisture Transport over South America

2

Wet season Dryseason

GPCP monthly means and ERA-Interim (we also use ERA40)

Page 3: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Aerial

Rivers

EGU General Assembly

Page 4: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Aerial Rivers

April 3-8 2011 EGU General Assembly 4

W =1

gqdp

0

ps

Precipitable water:

is analogous to the height of a column of liquid,multiplied by an equivalent column speed it gives the column discharge.

Page 5: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

A Lake of Moisture over Amazonia

April 3-8 2011 EGU General Assembly 5

Page 6: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Aerial Rivers and Lake (wet season)

EGU General Assembly 6

Page 7: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Questions we’ve been asking ourselves :

Is Amazonia a source of moisture for the atmosphere? When? Where? – There has been much speculation on this issue because of measurements showing a moister atmosphere over the

forest than over the ocean.

What is the total aerial river discharge into the subtropical rainfall areas?

What’s the importance of moisture from Amazonia to this flow?

April 3-8 2011 EGU General Assembly 7

Page 8: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Amazonia, source of moisture?

The basin cannot be systematically a source of moisture or it would dry out.

For the whole basin RT>0 always.

If then and if , then

April 3-8 2011 EGU General Assembly 8

P − E = RT + S

P − E < 0

S < −RT < 0

S > 0

P − E > RT > 0

Page 9: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

When soil moisture is increasing in the basin as whole we expect it to be a sink of moisture. (There could be variability in space)

It is worth investigating if, in the drier season, or in the months following it the basin acts as a source of moisture.

April 3-8 2011 EGU General Assembly 9

Page 10: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

One option is to use the balance equation for atmospheric water vapor as put by Peixoto & Oort 1992.

Time variation of precipitable water is being dismissed as small.

But the divergence field requires validation.

April 3-8 2011 EGU General Assembly 10

P − E = −∇(QV )

Page 11: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Rainfall and Divergence

April 3-8 2011 EGU General Assembly 11

Page 12: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

April 3-8 2011 EGU General Assembly 12

Divergence of the vertically integrated moisture transport for ERA40 (left, 1980-2001) and ERA-Interim (right, 1989-

2008) data.

Page 13: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

Interim

April 3-8 2011 EGU General Assembly 13

Page 14: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

ERA40

April 3-8 2011 EGU General Assembly 14

Page 15: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

EGU General Assembly

Summary

Both data sets show flow from Amazonia and from the Atlantic to be similar in mean magnitude.

Flow from Amazonia has larger spread and therefore a larger effect over the variability of the aerial river discharge.

The contribution from soil evaporation follows closely in intensity. -> ”Only” moistens the air. April 3-8 2011 15

Page 16: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

EGU General Assembly

Summary

It would be very interesting to compare with evaporation data.

April 3-8 2011 16

Page 17: Aerial Rivers and Lake, Subtropical Rainfall and soil Evaporation Josefina Moraes Arraut, C. Nobre, H.M.J. Barbosa, A. Marengo, CCST - INPE EGU General

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