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Annual Report 2000-2001
Scientific Research
Monsoon and Tropical Climate (MONTCLIM)
The Monsoon and Tropical Climate Programme
is directed towards undertaking studies on monsoon climate
variability/change, modelling atmospheric processes and technology
development for atmospheric science research. In order to
study the effect of weather and climate in tropics, efforts
are being made to improve parameterisation of land-ocean-atmospheric
processes in the Atmospheric General Circulation Models (AGCM).
Climate modelling:
The spatial and temporal variability of error
growth rates in predicting climate system using coupled ocean
atmosphere model indicated that the fast growth rate is characteristic
of small scales of motion, independent of seasons. Also, the
initial errors in small scale quickly travel to the dominant
mode in spring, while the coupled system does not allow it
to do so in autumn or winter. A conceptual model to study
how the intra-seasonal oscillations (ISO) could influence
the seasonal mean monsoon has been developed. The evolution
of 30-60 days mode shows that the ISO is characterised by
a systematic northward propagation of the tropical convergence
zone. Whereas, 10-20 days mode is rather regional in character
with its significant anomalies confined to the Bay of Bengal.
Several numerical experiments were undertaken with general
circulation model at different resolutions (T63L19, T42L09
& T80L18) using different types of envelope orography
to simulate the large scale features of Indian summer monsoon
and movement of tropical cyclones. The NCMRWF operational
model (T80L18) results indicate that performance of 2-D filters
is superior to 1-D filter.
The development of the climate version of the NCMRWF model
has been completed. The initial results indicated that the
model realistically simulates most of the major features of
the Indian summer monsoon.
Tropical Cyclone Simulation:
A multi-level axi-symmetric primitive equation
model has been developed and tested with different cumulus
parameterisation schemes, to study the evolution of cyclonic
circulation over Bay of Bengal. Sensitivity experiments indicated
that the increase of sea surface temperature contributes to
faster development and stronger cyclonic systems. One numerical
experiment using a Mesoscale Model (MM5) was carried out to
simulate the cyclonic systems and the track positions over
Bay of Bengal occurred during November 1996. The results on
strength and track of the cyclone are encouraging.
The numerical experiments using axi-symmetric model of tropical
cyclone with Arakawa-Schubert scheme for convection indicated
that (a) the size of the incipient system (about 250 km radius)
play an important role in the process of intensification;
(b) a basic characteristic of intensifying system is centrally
organised convection at the initial state whereas non-intensifying
systems exhibited large scale divergence activity in the core
region at the initial stage; (c) strong correspondence between
intensification and sustained and organised cloud activity
near the center, and (d) the scale selective intensification
appears to arise from a delicate combination of the vertical
distribution of temperature and humidity.
Land-Atmosphere:
Preparation of monthly mean gridded (1o X 1o)
data sets on land surface characteristics of the Indian Subcontinent
is completed. A one-dimensional land surface scheme of energy,
momentum, water and CO2 exchanges between the atmosphere and
land surface has been developed. The sensitivity experiments
demonstrate that vegetation exerts a mitigating influence
on both the land surface and atmosphere. Experiments with
a `Regional Atmospheric Modelling System (RAMS)' suggest that
the model performs better with an interactive biosphere-hydrological
land surface scheme. The impact of interactive hydrology vis-a-vis
specified hydrology on the seasonal mean simulation using
Climate Community Model indicated that surface processes play
a significant role in the simulation of the monsoon features.
The quality checked data generated during the `Land Surface
Processes Experiment (LASPEX)' over Sabarmati River Basin
in Gujarat are made available to the scientific community
for further analysis. The initial scientific results presented
at the LASPEX workshop are under publication. The data sets
are utilised to validate different land surface parameterisation
schemes in a 1-D soil-vegetation boundary layer model, 2-D
Meso-scale model and a 3-D limited area model. The seasonal
variation in radiation flux, soil heat flux, sensible and
latent heat fluxes are well simulated by the models. The impact
studies indicated that inclusion of land surface processes
scheme in 3-D model enhanced the predicted latent heat flux
and sensible heat flux gradients over land and these gradients,
there by increased the low-level convection. These results
further demonstrate the importance of the parameterisation
of the land surface processes in the short-range prediction/simulation
of summer monsoon circulation features and rainfall over India.
Ocean-atmosphere:
A global ocean general circulation model was
developed for the first time in India. The model is able to
respond to wind stress and reproduces the structure of temperature,
salinity and density fields. Further, model simulation indicated
the realistic intra-seasonal as well as interannual variations
of sea surface temperature. The development of a coupled ocean-atmospheric
model is in progress. A simple model of the meridional circulation
has been formulated. Trail integration of the model show that
the model tracer fields are sensitive to the meridional velocity
field. The work related to the seasonal variations of the
meridional circulation, in the upper 400 meters of the ocean
is in progress. Surface flux measurements in the Ocean-Atmosphere
boundary layer during INDOEX (Indian Ocean Experiment) field
phase were undertaken. A 4-meter micro meteorological tower
with sensors mounted at 3-levels was installed on the ship.
Both fast and slow sensors were used. The data collected are
being analysed.
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Agrometeorology
Field experiments and modelling studies on
the effect of weather and climate on the crop growth, pest
and disease development and yields are being undertaken under
this sub-programme. The data generated has been used to develop
sub?routines for agrometeorological processes, testing and
validation. Initiated studies on land surface processes over
Wheat crop at Anand. Modelling the effect of weather and climate
on cotton growth and yield is underway. A weather based Rice
blast disease forecasting system in the Kangra region of Himachal
Pradesh was developed.
Successfully completed the initial development of an agrometeorological
data bank at the Central Research Institute for Dryland Agriculture
(CRIDA), Hyderabad. The facility is to collect, compile and
archive various types of crop and weather data generated under
agrometeorology projects supported by Indian Council of Agricultural
Research and DST. New projects were initiated to study the
nitrogen flux from rice wheat system in northwest India, methane
emission from rice fields in the northeastern region, agroclimatic
variability in the Uttar Pradesh - Bihar plains and modelling
environmental modulations in rate of development of Soybean
genotypes. Experiments on methane emission from natural wet
lands are under progress.
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Radio Acoustic
Sounding System (RASS)
A multi-institutional supported project on the
indigenous development of Wind Profiler /Radio Acoustic Sounding
System has been completed. The system will have the ability
to provide temperature profile (up to 5 km) and wind profile
(up to 10?16 km) in the atmosphere. The initial validation
tests of system have been done with available upper air wind
data. The results are encouraging and needs further tuning.
The Project Advisory and Monitoring Committee suggested that
this prototype system to be permanently installed at Pune
to carry out detailed validation tests and specific experiments
by the atmospheric scientists in collaboration with India
Meteorological Department. Accordingly, arrangements were
made to shift the system to Pune. The site developmental work
to install the system is in progress.
Indian Climate
Research Programme (ICRP)
The objectives of the Indian Climate Research
Programme (ICRP) are, (i) analysis of observational data from
ground-based, ship-based and satellite-based measurements,
(ii) modelling studies with coupled ocean-atmospheric general
circulation models and (iii) identification of the climate
component of agricultural productivity, impact of climate
on environment and climate change, etc. A number of projects
were evolved and supported.
The first field observational experiment under the ICRP, called
the Bay of Bengal Monsoon Experiment (BOBMEX), was carried
out successfully. BOBMEX was aimed at measurements of important
variables of the atmosphere, ocean and their interface to
gain deeper insight into some of the processes that govern
the variability of organised convection over the Bay. Simultaneous
time series observations were carried out in the northern
and southern Bay of Bengal from ships and met ocean buoys.
About 80 scientists from 15 different institutions in India
collaborated during the BOBMEX to make observations in most
hostile conditions of the raging monsoon. The initial results
indicated the following.
During the BOBMEX field phase there were several active spells
of convection over the Bay, separated by weak spells. Observations
with high resolution rediosonde, launched for the first time
over northern Bay, showed that the magnitudes of the Convective
Available Potential Energy (CAPE) and the Convective Inhibition
Energy (CINE) were comparable to those for the atmosphere
over the West Pacific warm pool. CAPE decreased by 2-3 kJkg-1
following convection, and recovered in a time period of one
or two days. The surface wind speed was generally higher than
8 ms-1. The thermohaline structure as well as its time-evolution
during the BOBMEX field phase was found to be different in
the north Bay from the south Bay. Over both the regions the
sea surface temperature (SST) and sea surface salinity decreased
during rain events and increased in cloud free conditions.
Over the season as a whole, the upper layer salinity decreased
for the north Bay and increased for the south Bay. The variation
in SST during 1999 was found to be of smaller amplitude than
in 1998. The quality checked atmospheric and oceanographic
data sets were provided to the scientific community. Further
analysis of the surface fluxes and currents is expected to
give insight into the nature of coupling. Twelve research
papers based on the data analysis from BOBMEX-Pilot study
were published as a special issue of the Proceedings of the
Indian Academy of Sciences, Earth and Planetary Sciences (Vol.
109, No.2. June 2000).
Prepared the science plan on Arabian Sea Monsoon Experiment
(ARMEX). The technical programme to carryout ARMEX during
2002 is under preparation. Initiated studies on (a) Monsoon
dynamics, energitics and variability, (b) Development of optimised
atmospheric general circulation model, (c) Impact of natural
processes and anthropogenic activities on the atmospheric
chemistry, (d) ENSO-Snow-Monsoon interactions and (e) Differential
absorption LIDAR sensing of Ozone. Fortnightly samples of
atmospheric precipitation and ground water were collected
from 12 locations in and around Mangalore (Karnataka). Measurements
of physiochemical parameters and aerosols are in progress.
The development of a coupled ocean-atmospheric model is in
progress.
A brainstorming session on `Weather Modification Research'
was organised at Indian Institute of Tropical Meteorology,
Pune. Expert comments on the technical paper on `Forest fire
and transboundary haze pollution' were obtained to evolve
a new programme. A training workshop on `Agroclimatic analysis
and Database Management Techniques' was organised for 20 young
scientists for two weeks duration at CRIDA, Hyderabad.
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