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EARSeL Newsletter - EARSeL, European Association of Remote ...

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<strong>EARSeL</strong> <strong>Newsletter</strong> September 2002 - Number 51<br />

28<br />

ters on the US DMSP (Defence Meteorological<br />

Satellite Programme) satellites up to F-<br />

14, launched in April 1997.<br />

In the opinion <strong>of</strong> the reviewer, the most interesting<br />

part <strong>of</strong> the book is the final chapter,<br />

dealing with "microwave observations<br />

<strong>of</strong> processes in the ocean-atmosphere system".<br />

It presents results <strong>of</strong> experiments carried<br />

out from ships and aircraft, <strong>of</strong> the<br />

phenomena previously dealt with. Internal<br />

waves were studied in a cruise on the Indian<br />

Sea (1981), with a radiometer-scatterometer<br />

at 37 GHz (vertical polarisation) and a<br />

radiometer at 1.7 GHz (horizontal polarisation)<br />

operated at an angle <strong>of</strong> incidence <strong>of</strong><br />

75º. Another experiment was carried out<br />

with a 37 GHz radiometer (vertical polarisation)<br />

and a high-resolution echo-sounder<br />

recording internal solitons in the Sea <strong>of</strong><br />

Japan (1981). Still other experiments were<br />

carried out in the Atlantic Ocean (near<br />

Long Island) in a Joint USA / Russia Internal<br />

Wave <strong>Remote</strong> Sensing Experiment<br />

(JUSREX, 1992) with the "aircraft laboratory<br />

Tupolev-134" equipped with a real-aperture<br />

radar at 13 GHz and radiometers at<br />

1.6, 3.9, 20 and 37 GHz. Rather convincing<br />

results are presented and commented on.<br />

One section deals with the surface effect <strong>of</strong><br />

rain. Rain changes both the surface salinity<br />

and occasionally also its temperature,<br />

which changes the ripple structure on the<br />

ocean surface and thereby the microwave<br />

thermal emission. Examples show that the<br />

effect is limited in time to an hour or so.<br />

Ship-borne measurements (1984) with a radiometer<br />

system at 48, 37, 34 and 20 GHz, all<br />

vertical polarisation, and another channel at<br />

37 GHz, horizontal polarisation, reveal the<br />

rather surprising result that the "relic rain" is<br />

observed at all frequencies except 20 and 37<br />

GHz, vertical polarisation.<br />

The author spends a few pages discussing<br />

the reason for the observation that the effect<br />

is seen on one frequency and not another,<br />

only 3 GHz away – unfortunately not very<br />

convincingly. In contrast, a so-called tropical<br />

shower (20 mm/h) may be seen on all<br />

frequencies and polarisations: at 34 GHz,<br />

horizontal polarisation the brightness temperature<br />

increases by more that 100 K.<br />

Similarly, a frontal zone was detected by<br />

the ship-borne radiometer / scatterometer<br />

at 37 GHz in the Pacific Ocean (1983), revealing<br />

strong ‘signatures’ <strong>of</strong> more than 20<br />

K and 10 dB in one case, and about 3 dB in<br />

another. An oceanic synoptic ring was<br />

recorded from a radiometer on a TU-134 research<br />

aircraft at 37 and 48 GHz, but not at<br />

20 and 75 GHz (1990). The cyclone Warren<br />

(1984) gave surface effects that were observed<br />

at 48 and 34 GHz, but not on 20 and<br />

37 GHz (all vertical polarisation). Finally,<br />

SMM/I data (1997) revealed an interesting<br />

signature in a 600 kilometres long area<br />

along the continental break in the northern<br />

part <strong>of</strong> Norwegian Sea.<br />

In some <strong>of</strong> the cases presented, the observations<br />

are supported by simultaneous oceanic<br />

and meteorological data. In other cases<br />

they are discussed in the context <strong>of</strong> oceanic<br />

research in the area in question, <strong>of</strong>ten carried<br />

out by Russian research vessels.<br />

This interesting but specialised book is a revision<br />

<strong>of</strong> a previously published book<br />

(1994, in Russian) with some additions <strong>of</strong><br />

which the SMM/I data are worth mentioning.<br />

The observations presented are thoroughly<br />

discussed in an oceanic context,<br />

referring to a great number <strong>of</strong> relevant research<br />

papers. In fact, the extensive list <strong>of</strong><br />

references (over 275) is a valuable source <strong>of</strong><br />

information about oceanic and meteorological<br />

research carried out in Russia, many <strong>of</strong><br />

which have been translated into English.<br />

The book has some shortcomings, in that<br />

the language is rather elaborate; at few<br />

places sentences (apparently interpreted<br />

from Russian) are difficult to understand<br />

by another foreigner.<br />

5.2 Book: study <strong>of</strong> Kara Sea, Russian<br />

Arctic<br />

Polar Seas Oceanography: An Integrated Case<br />

Study <strong>of</strong> the Kara Sea. Authors: Vladimir A.<br />

Volkov, Ola M. Johannessen, Victor E.<br />

Borodachev, Gennadiy N. Voinov, Lasse H.<br />

Pettersson, Leonid P. Bobylev and Alexei V.<br />

Kouraev. May 2002. Praxis Publishing Ltd.<br />

496 pp., including 12-page colour section.<br />

ISBN: 3-54042-969-7. List price: 104.50 Euros.<br />

The Kara Sea <strong>of</strong> the Russian Arctic, with its<br />

unique oceanographic regime, is a site <strong>of</strong>

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