Вестник Каспия №4/2008 Caspian Sea Bulletin От Редакции журнала «Вестник Каспия»



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Introduction


Satellite altimeters are capable of providing a detailed picture of sea level and track its change regularly. The launch of the TOPEX/Poseidon in 1992 provided the greatest impetus for satellite altimetry research in the 20th century. Its launch was followed by the Jason-1 (2001) and Jason-2 (2008). ESA satellites were launched in 1991, 1995, 2002 (ERS-1, ERS-2, Envisat) and the US Navy Geosat Follow-On was launched in 1998. Whilst several of these missions are still in active orbit and expected to continue operation for the foreseeable future, new missions are planned to be launched by space agencies over the next few years (CryoSat-2, AltiKa, Sentinel-3) [1, 2]. Satellite altimetry is recognised as an essential component of the earth observing systems under international programmes such as GEOSS. Data actively collected at sea are necessary to ensure that satellite remotely sensed data are properly calibrated and validated. Only with a reliable calibration/validation process can changes observed in the altimeter-derived sea levels be interpreted as either changes in the instrument or changes in the environment.

The Caspian Sea is the biggest enclosed body of water on Earth, with a coastline approximately seven thousand kilometres long. Situated in a natural depression, below mean sea level, it receives water from freshwater inputs, but has no opening to the oceans. The Caspian Sea is subject to significant water level fluctuations which have had serious consequences for the region, displacing thousands of shoreline inhabitants, destroying investments in industry and infrastructure. Sea level in the Caspian Sea is clearly a topic of public concern to all five surrounding countries (Azerbaijan, Republic of Iran, Kazakhstan, Russian Federation and Turkmenistan). In addition to the danger posed to oil fields and coastal infrastructure, the water level fluctuations result in changes in a number of processes such as: water regime; dynamics and chemical composition of groundwater; structure and productivity of biological communities in the littoral [3, 6].

The network of operating stations along the coast of the Caspian Sea has sharply declined to such an extent that many areas are no longer monitored. The present situation is that the sea level station infrastructure is in a very poor state and is continuing to deteriorate, having an impact on strategic planning and management decisions at both national and regional levels (Fig.1). As a result, the infrastructure is obsolete and, in many cases, the level of technical expertise is very low. There is pressing need for improved systematic sea level

(a)


(b)


Fig.1. A view of the sea level station (a) and measuring device (b) in Baku.

Рис.1. Вид уровнемерного поста (а) и измерительного оборудования (б) в Баку.

observations with high accuracy and resolution in the Caspian Sea and for the creation of a regional database as a basis for a reliable assessment of changes and sound scientific research. There is also a need for correct operation of sea level stations to ensure data quality and reliability. At present, no stations are maintained to GLOSS standards and therefore none is really usable for satellite altimetry calibration. In addition, no cross national uniform geodetic levelling network exists along the coasts. The consequence is that the measurements of sea level at different sites are not comparable.

The ALTICORE initiative and synergies


The project named ALTICORE (www.alticore.eu) has been funded by INTAS program (European Community) for a period of two years - beginning 1 December 2006, through a concerted action, coordinated by Consiglio Nazionale delle Ricerche (CNR, Italy), and bringing together teams from Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS, France), National Oceanography Center, Southampton (NOCS, UK), P.P. Shirshov Institute of Oceanology (SIO, Russian Federation), Geophysical Center (GC, Russian Federation) and Institute of Geography (IG, Azerbaijan) [4, 5]. The main objective of ALTICORE is to encourage the operational use of satellite altimetry over coastal areas, by improving the quality and availability of coastal altimetry data, with particular reference to some European seas, including the Caspian Sea (Fig. 2). The limited budget of ALTICORE does not permit the establishment of the in situ-based component for the satellite altimetry validation. The plan of scientific exchange visits has permitted to inspect suitable sites where to potentially install measuring instrumentation. At the same time, the LEGOS team received some funding to buy an equipment to measure sea level. There were conditions for the establishment of a funding synergy between ALTICORE and LEGOS initiatives.

This report describes a field mission to install a pilot sea level monitoring station at Port Absheron, Baku, Azerbaijan (Fig.3, 4), that was held on 8-13 June 2008. The intention of this technical mission was (1) to deploy a bottom pressure owned by LEGOS at the site identified during a previous inspection visit in September 2007; (2) to perform a geodetic levelling campaign, including GPS measurements at land and sea. It is expected that we will be able (1) to collect an accurate record of in situ sea level measurements at high temporal resolution; (2) to assess the impact of local conditions in terms of weather and morphology; (3) to decide if the site is good candidate for installation of a permanent calibration/validation (cal/val) site for satellite altimetry.







(a) (b)






(c) (d)

    Fig. 2. Satellite altimetry ground track coverage from Jason-1 (a), Envisat (b), GFO (c) and Topex/Poseidon (2002-2005) (d) in the Caspian Sea.

    Рис.2. Треки спутников Jason-1 (a), Envisat (b), GFO (c) и

    Topex/Poseidon (2002-2005 гг.) (d), проходящие по акватории Каспийского моря.



Fig.3. Satellite view of Port Absheron (shown by arrow) and a bridge to Pirallahi (Artyom) Island

(source Virtual Earth).

Рис.3. Спутниковое изображение порта Апшерон (указано стрелкой) и моста на о. Пиралахи (Артем).

Fig.4. View of Port Absheron.

Рис.4. Вид Апшеронского порта.



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