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A monsoon in more than two halves

August 4, 2015 by Climate portal editor Leave a Comment

ICP_imd_forecast_20150804

Less rain for the remaining two months of the typical monsoon season of four months, but an overall season average that remains as it was forecast in June. This is the confusing monsoon update issued by the Earth System Science Organization (ESSO), the Ministry of Earth Sciences (MoES) and the India Meteorological Department (IMD).

There are aspects of IMD’s treatment of the monsoon season that need correction in our view. One is the long range forecast and its updates. Specific to this update, we are at the halfway stage of what is typically considered the four month monsoon (this too needs revision, as April and May rains were not the usual ‘unseasonal’ passing showers). However, any downward revision of the rainfall average for August and September ought to be an overall downward revision of the season, particularly as June-July have seen very uneven rain.

Consider the highlights of the updated monsoon forecast:

* Quantitatively, the rainfall over the country as a whole during the second half of the season (August to September) is likely to be 84% of LPA with a model error of ±8%.
* The rainfall during August is likely to be 90 ± 9% of LPA as was forecasted in June.
* The season (June to September) rainfall over the country as a whole is likely to be 88% of LPA with a model error of ±4% as was forecasted in June.

ICP_imd_points_20150804We make our criticism constructively, for a significant amount of the material India Climate Portal puts out through our website and our twitter account is taken from the public products released by IMD, ISRO and the Ministry of Earth Sciences, and we fully appreciate the quality of work and commitment of these agencies.

The national mean rainfall (“country as a whole”, as the IMD forecasts call it) must be abandoned as it does not represent the meteorological diversity of a very large country. Each of the 36 met sub-divisions is affected in different ways by the El Nino Southern Oscillation, the Indian Ocean dipole, the Madden-Julian Oscillation and other hemispheric phenomena.

There is no need for this simplification, which in fact achieves the opposite of timely accuracy.
The media in particular (television and radio, print, online) look for an overall message and, without guidance from authorities, picks up ‘top line’ messages that are of little or no use at the district and taluka level, and also for towns and cities. The question for IMD is rather: how will variability in monsoon together with the strengthening El Nino affect local outlooks for August to October. That is why we advocate monthly outlooks for the 36 met sub-divisions, to begin in May and to run until October (that is, half the year and not a third of the year), primarily to prepare local administrations for all possible scenarios.

There is no reason why this cannot be the approach. The Ministry of Earth Sciences coordinates the observation network (satellites included, and our agencies ISRO and NRSC are heavily involved), the IMD uses these data together with a very extensive network of weather stations all over India. The output is excellent quality and in the public domain. Because the meteorological services in India have historically been designed to aid and guide agriculture and cultivation, the agri-met bulletins, alerts and products are copious. Hence IMD/MoES listens to the needs of the agricultural departments and, more recently, disaster management agencies. Unfortunately, the interface with public is still minimal, which this central government can also easily remedy.

Filed Under: Latest, Monsoon 2015 Tagged With: 2015, climate, earth sciences, El Nino, forecast, IMD, India, ISRO, monsoon

Earth, sea, sky, El Niño

June 17, 2015 by Climate portal editor Leave a Comment

ICP_20150617_sm

Eight-and-a-half degrees north of the equator is where the peninsula of India meets the ocean. Our country stretches across 29 degrees of latitude but it is in the vast watery realm south of Kanyakumari that the Indian summer monsoon is brewed, slowly and inevitably. Over twice as many lines of latitude stretches the Indian Ocean, its equatorial belt and then its southern reaches, which continue into the deep and icy girdles of water around Antarctica.

From this vast aqueous quarter-planet the vapours are gathered, and these swirls of airborne water then look for the winds to transport them, first towards the mid-southern latitudes (Madagascar lies astride these, but they are are still a full ten degrees south of the lower coasts of Java) and then in the equatorial trough that spins like a motor. From here these enormous masses of water – half again the size of India at times – are hurled as if in slow motion towards our western coast.

And so to gauge imperfectly whether the wind lords of the farther Indian Ocean have decided to be kind to us we rely nowadays on our eyes in the sky, our weather satellites. What they tell us now is coded in electronic chirps made intelligible by the meteorologists and climatologists of the Indian Meteorological Department, the Ministry of Earth Sciences, the Indian Institute of Tropical Meteorology and the National Centre for Medium Range Weather Forecasting.

Our Indian summer monsoon is amongst the most complex of the planet’s earth-sea-sky interactions. We are told by the scientists, when they disengage from their equations, that the land retains a shorter climate ‘memory’ than the ocean. We are introduced to meridonal termperature gradients and seasonal migration of the inter-tropical convergence zone.

There is an abundance of exotic nomenclature: the Mascarene High, the orographic influence of the East African Highlands, the momentum of the Somali Jet, the ventilation effect of poleward precipitation. And then there is the hot star of the equatorial deeps, El Niño himself, whose domain is the central Pacific and who, when he awakes, demands that the equatorial Indian Ocean obey. He has awoken this year, but the ocean named after us is as unruly as ever.

When will El Niño’s whip really crack? The best models of the climate scientists cannot truly tell us. They and their teraflop calculating machines can only posit what is measured, and what remains unmeasured is still far greater. What we do however know about El Niño is that he does tend to suppress the monsoon. But this year’s El Niño may not resemble one of an earlier year, for where El Niño arises and rules is as important as when. Where the ocean surface warms up (several thousand kilometres parallel to the equator, several hundred kilometres wide) unusually strong rising air flows result.

When these flows descend (as they eventually must) they are generally dry and stable, and so the opposite of conditions needed for or monsoon rains. If they descend far away from India (as happened in 1997-98 when they dropped back into the eastern Pacific) our ocean will deliver and our monsoon will roll in. If they descend in the middle of the Pacific (which happened in 2002) our monsoon will resent the interference and hide. But El Niño is awake and pacing the Pacific. We must hope he does not look too far westwards. (RG)

Filed Under: Blogs, Monsoon 2015 Tagged With: Climate Change, earth science, El Nino, ENSO, India, Indian Ocean, monsoon, planet

North-East India reels under rain

June 10, 2015 by Climate portal editor Leave a Comment

A village threatened by rising floodwaters in Arunachal Pradesh. Image: Arunachal Times

A village threatened by rising floodwaters in Arunachal Pradesh. Image: Arunachal Times

Torrential rain in north-east India has caused rivers to swell with water, several above their danger marks, and has isolated entire districts. Reports from Arunachal Pradesh, Assam and Meghalaya – states that have experienced heavy to very heavy rain over the last four days – indicate a situation for the region that is approaching an emergency.

#monsoon2015 Next 6 days' rain for NE India. Red hues are 50-90 mm/day. Intensity lessens from 15th #Assam #Arunachal pic.twitter.com/YWEJ2BQCFD

— Indiaclimate (@Indiaclimate) June 10, 2015

A father carries his child to school in waterlogged Anil Nagar, Guwahati. Image: PTI/Express

A father carries his child to school in waterlogged Anil Nagar, Guwahati. Image: PTI/Express

The Indian Express has reported that thousands of people in Assam have been affected with several rivers, including the Brahmaputra, overflowing their banks. The rivers have breached embankments, inundated villages and damaged standing crops, affecting over 80,000 people, according to the state disaster management body.

The Arunachal Times has reported that the districts of Upper Siang, Dibang Valley and Anjaw are cut off from the region due to torrential rainfall which has triggered flash floods and landslides at various locations. Major rivers in Arunachal Pradesh including the Siang are in spate. The Echo of Arunachal has reported that Pasighat, the state’s oldest administrative town, is under threat of inundation and the provision of water and electricity to town inhabitants has stopped.

Filed Under: Current, Monsoon 2015 Tagged With: Arunachal, Assam, flood, India, Meghalaya, monsoon, North-East, river

Being prudent about forecasts

June 3, 2015 by Climate portal editor Leave a Comment

ICP_pre-monsoon_seasons_2011-15_sm

The Earth System Science Organisation (ESSO), Ministry of Earth Sciences (MoES) and the India Meteorological Department (IMD) released their second long range forecast for monsoon 2015 on 2 June. The ‘headline’ message is that rainfall for the June to September monsoon season is very likely to be 88% of what is normal for the season.

The forecast has been seized upon by various quarters as having serious implications for the production of crop staples (and therefore for food security), for farmers’ livelihoods, for consumer prices and for the availability of water. These are all valid and important aspects that depend entirely or substantially upon the summer monsoon.

But, the IMD, the ESSO and the MoES do not make statements and forecasts on these aspects. They are concerned with what the climatological data and signs point to, and that is what they have told us. How the forecast relates to important aspects of food, farm incomes, water resources and food stocks relies on interpretations. Our advice – to the media, to government agencies and to the private sector – is to go slow on drawing conclusions and when conclusions are required, to make them incrementally.

The wettest pre-monsoon season (March to May) for five years.

The wettest pre-monsoon season (March to May) for five years.

Using the handy graphic here, (887KB) we also point out that the pre-monsoon season (March to May) for 2015 has been the wettest in five years. In several meteorological sub-divisions, excess rain has been recorded during this pre-monsoon season. In several districts, the annual rainfall total has already been reached, even before the typical monsoon season of June to September.

This ought to be warning enough to us to be sparing with deciding how forecasts will affect us. The ESSO, IMD and MoES have repeated, in their second long range forecast, that 2015 is an El Niño year which only means that as this sea temperature phenomenon waxes and wanes though the remainder of 2015, so too will the monsoon system react.

It is best to judge our Indian summer monsoon a week at a time, keeping in mind crop calendars and how much water our reservoirs hold. It is always prudent to take precautions such as rationing water (even when it is raining), especially in towns and cities. Likewise, district administrations will do well to assess their local supplies of food staples and match these figures with what food staples their districts are likely to produce during a monsoon whose reliability has now been written off.

The second long range forecast for monsoon 2015 is available here, and the Hindi text can be found here.

Filed Under: Monsoon 2015, Reports & Comment Tagged With: 2015, climate, consumer price, crop, El Nino, farm, food stock, forecast, IMD, India, meteorology, monsoon, sea surface temperature, water

How El Niño plans to hijack monsoon 2015

May 26, 2015 by Climate portal editor Leave a Comment

ICP_El_Nino_monsoon_20150526_smWhether the monsoon starts off on time, whether the June, July, August and September rainfall averages are met, and whether the seasonal pattern of the monsoon is maintained are expectations that must now be set aside.

According to the Climate Prediction Center’s ENSO probability forecast, there is a 90% chance that El Niño conditions will prevail through June to August of the northern hemisphere and a more than 80% percent chance El Niño will last throughout all of 2015.

The Ministry of Earth Sciences El Niño/La Nina, Indian Ocean Dipole Update (10 May 2015)

The Ministry of Earth Sciences El Niño/La Nina, Indian Ocean Dipole Update (10 May 2015)

What this means, especially when record warm global atmospheric temperatures (because we in South Asia and our neighbours in East Asia have continued burned coal as if the resulting CO2 and soot simply doesn’t exist) are being set, is the remaining months of 2015 – the monsoon period included – will bring strange, dangerous and extreme weather. We have already seen that over the last week, with the death toll from the heat wave having crossed 550.

For the first time since 1998 – ­the year of the strongest El Niño on record, which played havoc with the
world’s weather patterns and was blamed for 23,000 deaths worldwide – ­ocean temperatures in all five El Niño zones have risen above 1 degree Celsius warmer than normal at the same time. That is read by climatologists and ocean scientists as presaging an El Niño that is moderately strong to strong. The forecast models updated in May are now unanimous that El Niño is going to keep strengthening through the rest of 2015. (See also the official forecast from the USA’s government climate science agency.)

El Niño’s home is in the tropical eastern Pacific, but we in India need to watch the waters to our south very closely. New research published in the journal Nature Geoscience has examined records going back to 1950 and noticed that Indian Ocean absorbed heat at a low level until 2003. Thereafter, the excess oceanic heat in the Pacific Ocean found its way through the Indonesian archipelago and into the Indian Ocean. This is the gigantic reservoir of watery heat that is going to dictate terms to our summer monsoon, or what our school textbooks call the south-west monsoon.

It is a worry for the entire South Asian region – India, Pakistan, Sri Lanka, Bangladesh, Nepal, the Maldives, Burma, Afghanistan and Bhutan. That is why when the Forum on Regional Climate Monitoring-Assessment-Prediction for Asia (FOCRA) issued its seasonal outlook for June to August 2015 it predicted weaker than normal Indian summer and East Asian monsoons. Precipitation over land is influenced by external factors such as the El Niño Southern Oscillation (the ENSO), the ‘Indian Ocean Dipole’, the ‘Arctic Oscillation’, and so on.

There may be a “timely onset” of the monsoon, as the venerable IMD is used to saying, but that doesn’t mean our troubles are over. Far from it.

Filed Under: Latest, Monsoon 2015 Tagged With: Bangladesh, Bhutan, El Nino, ENSO, India, Indian Ocean, Maldives, monsoon, Nepal, Pacific, Pakistan, Sri Lanka

Celsius surprises in 57 cities

May 21, 2015 by Climate portal editor Leave a Comment

ICP_57_cities_temp_top

The middle of February is when the chill begins to abate. The middle of May is when the monsoon is longed for. In our towns, district headquarters and cities, that climatic journey of 90 days is one of a steady rise in the reading of the temperature gauge, from the low 20s to the mid 30s.

This large panel of 90 days of daily average temperatures shows, in 57 ways, the effects of the rains that almost every district has experienced during the last two months. For each city, the curved line is the long period ‘normal’ for these 90 days, based on daily averages. Also for each city, the second line which swings above and below the ‘normal’ is the one that describes the changes in its daily average from February to May 2015.

[You can download (1.52MB) a full resolution image of the panel here.]

Where this second line crosses to rise above the normal, the intervening space is red, where it dips below is coloured blue. The patches of red or blue are what tell us about the effects of a lingering winter, or rains that have been called ‘unseasonal’ but which we think signal a shift in the monsoon patterns.

Amongst the readings there is to be found some general similarities and also some individual peculiarities. Overall, there are more blue patches than there are red ones, and that describes how most of the cities in this panel have escaped (till this point) the typical heat of April and May. The second noteworthy general finding is that these blue patches occur more frequently in the second half of the 90 days, and so are the result of the rainy spells experienced from March to early May.

Hisar (in Haryana) has remained under the normal temperature line for many more days than above or near it. So have Gorakhpur (Uttar Pradesh), Pendra (Chhattisgarh), Ranchi (Jharkhand), Nagpur (Maharashtra) and Jharsuguda (Odisha).

On the other hand in peninsular and south India, the below ‘normal’ daily average temperature readings are to be found in the latter half of the time period, coinciding with the frequent wet spells. This we can see in Kakinada, Kurnool and Anantapur (Andhra Pradesh), Bangalore, Gadag and Mangalore (Karnataka), Chennai, Cuddalore and Tiruchirapalli (Tamil Nadu) and Thiruvananthapuram (Kerala). [A zip file with the charts for all 57 cities is available here (1.2MB).]

What pattern will the next 30 days worth of temperature readings follow? In four weeks we will update this bird’s eye view of city temperatures, by which time monsoon 2015 should continue to give us more blues than reds. [Temperature time series plots are courtesy the NOAA Center for Weather and Climate Prediction.]

Filed Under: Current, Monsoon 2015, Reports & Comment Tagged With: Anantapur, Andhra Pradesh, Bangalore, Chennai, Chhattisgarh, city, climate, Cuddalore, Gadag, Gorakhpur, India, Jharkhand, Jharsuguda, Kakinada, Karnataka, Kerala, Kurnool, Maharashtra, Mangalore, monsoon, Nagpur, Odisha, Ranchi, Tamil Nadu, temperature, Thiruvananthapuram, Tiruchirapalli, town, urban, Uttar Pradesh

Rain, climate, agriculture and Haryana

May 4, 2015 by Climate portal editor Leave a Comment

RG_ICP_rainfall_HAR_5Every one of Haryana’s 21 districts received excess rain for the period 1 March to 30 April 2015. As these rains have destroyed crops, including food staples, the need to compensate the affected farming families is now paramount. Relief and support are only useful when they are arrive quickly, and unlike administrative conditions two generations ago, state governments and district collectors today can consult data around the clock about conditions in districts and blocks.

Our infographic shows why the March and April rains in Haryana have had destructive effects. The average rainfall in a district of Haryana during this two-month period was 111.6 millimetres – most were in the range of 148 mm (like Ambala) and 81 mm (like Mahendragarh). However, the average for the two months, March and April, is 21.2 mm (Panipat and Faridabad are usually closest to this average).

RG_ICP_rainfall_HARAlthough the level of detail available at the district, and indeed even at the weather station level, is comprehensive, the Indian Meteorological Department’s rainfall quantity categories are not granular enough to describe what Haryana has experienced. (This is so for every state that has recorded what is called “unseasonal rain” in these months.)

Amongst the questions that remain unanswered concerning the ‘unseasonal rains’ phenomena – common to Haryana, eastern and western Uttar Pradesh, Bihar, Madhya Pradash, Rajasthan and Gujarat – is the matter of how much rain becomes excess over how many days? This meteorological sub-division (Haryana, Chandigarh and Delhi) normally receives 165 mm in July and 173 mm in August. Therefore, an average amount of 111.6 mm over two months is not a quantity that has surprised the agricultural community.

The matter is one of timing – which lapse the state administration needs to explain, as the weather forecasters first alert state administrations, which then relay alerts and advisories to district administrative staff. Between the claims for compensation for destroyed crops and the political point-scoring, the state government of Haryana has side-stepped the question: what did it do with the weather advisories it was given in March and April 2015?

For our series on the changing rainfall and climate patterns (the Haryana map is the first), we use six categories that begin with 10% above normal and extend to 1000% above normal. This method does better at identifying districts in which agriculture has been hit harder by unseasonal rains and stormy weather.

Filed Under: Latest, Monsoon 2015 Tagged With: 2015, agriculture, Climate Change, crop, district, farmer, Haryana, monsoon, rainfall

It’s to be a 93% monsoon says the IMD

April 22, 2015 by Climate portal editor 1 Comment

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The India Meteorological Department has just released it’s long-awaited forecast for the 2015 Indian monsoon. In terms of the quantity of rainfall over the duration of the monsoon season (June to September) the IMD has said it will be 93% of the ‘Long Period Average’. This average is based on the years 1951-2000.

What this means is the ‘national’ average rainfall over the monsoon season for India is considered to be 89 centimetres, or 890 millimetres. So, based on the conditions calculated till today, the ‘national’ average rainfall for the June to September monsoon season is likely to be 830 millimetres.

There are caveats and conditions. The first is that the 93% forecast is to be applied to the long period average for each of the 36 meteorological sub-divisions, and a ‘national average’ does not in fact have much meaning without considerable localisation. The second is that the forecasting methodology itself comes with a plus-minus caution. There is “a model error of ± 5%” is the IMD’s caution.

This first forecast and the model that the forecast percentage has emerged from are thanks to the efforts of the Earth System Science Organization (ESSO), under the Ministry of Earth Sciences (MoES), and the India Meteorological Department (IMD), which is the principal government agency in all matters relating to meteorology. This is what the IMD calls a first-stage forecast.

IMD_categories_201504As with all complex models, this one comes with several considerations. The ESSO, through the Indian Institute of Tropical Meteorology (IITM, which is in Pune), also runs what it calls an ‘Experimental Coupled Dynamical Model Forecasting System’. According to this, the monsoon rainfall during the 2015 monsoon season (June to September) averaged over India “is likely to be 91% ±5% of long period model average”. (The IMD forecast is available here, and in Hindi here.)

This is a lower figure than the 93% headline issued by the IMD. This too should be read with care as there are five “category probability forecasts” that are calculated – deficient, below normal, normal, above normal and excess. Each is accompanied by a forecast probability and a climatological probability (see the table). The maximum forecast probability of 35% is for a below normal monsoon, while the maximum climatological probability is for a normal monsoon.

As before, time will tell and the IMD will issue its second long range forecast in June 2015. Our advice to the Ministry of Earth Sciences and to the IMD is to issue its second long range forecast a month from now, in May, and also to confirm these forecasts two months hence in June, when monsoon 2015 will hopefully be active all over the peninsula.

Filed Under: Monsoon 2015, Reports & Comment Tagged With: 2015, climate, climatology, earth science, ESSO, forecast, IMD, India, meteorology, monsoon, weather

Follow the highs and lows of monsoon 2015

April 22, 2015 by Climate portal editor Leave a Comment

ICP_announce_20150422Our coverage of the ‘mausam’, the Indian summer monsoon of 2015, has begun. The unseasonal rains of March and April, which have proved so destructive to farmers, have shown why the conventional monsoon season must be widened. You will find all monsoon-related analysis, data and reports here.

We provide short, focused updates on weather trends. We strengthen the citizen’s understanding of the effects and impacts of climate change with relevant and jargon-free commentary.

We complement the Government of India’s excellent climate and weather monitoring services by advising what you can expect in your district or city, from unseasonal rains or the lack of it. Read our status reporting and analysis here on the India Climate Portal and follow our active twitter feed.

Filed Under: Announcements, Latest Tagged With: 2015, climate, data, forecast, India, monsoon, weather

A report card on monsoon 2014

October 1, 2014 by Climate portal editor Leave a Comment

RG_ICP_districts_table_201410From the first week of June 2014 until the middle of September 2014, there have been floods and conditions equivalent to drought in many districts, and for India the tale of monsoon 2014 comes from a reading of individual districts, not from a national ‘average’ or a ‘cumulative’. [This article was published by the newspaper DNA.]

Despite the advances made by our agencies in weather forecasting and climate monitoring, the science of meteorology still remains to be effectively distilled so that it can be used by citizens and, wherever possible, expanded and given context by ground-based observation and recording. One sector in which this does take place – albeit at a level still far below its potential – is agriculture. The reason is clear: our crop staples (the cereals, pulses, vegetables and fruit) have their individual calendars for preparation, sowing, tending and harvesting.

This line chart tells some of the tale. It shows that for the first six weeks of monsoon 2014, most districts recorded rain below their 'normals' for those weeks. The lines are percentile lines; they tell us what percent of districts recorded how much rainfall in a monsoon week relative to their normals for that week. This chart does not show how much rain - it shows distance away from a weekly normal for districts. The left scale is a percentage - higher percentages indicate how far above normal districts recorded their rainfall, negative numbers show us how far below normal their rainfall was. The dates (the bottom scale) are for weeks ending on that date for which normals and departures from normal were recorded. The P_01 to P_09 lines are the percentiles (10th to 90th) of all districts in every week.

This line chart tells some of the tale. It shows that for the first six weeks of monsoon 2014, most districts recorded rain below their ‘normals’ for those weeks. The lines are percentile lines; they tell us what percent of districts recorded how much rainfall in a monsoon week relative to their normals for that week. This chart does not show how much rain – it shows distance away from a weekly normal for districts.
The left scale is a percentage – higher percentages indicate how far above normal districts recorded their rainfall, negative numbers show us how far below normal their rainfall was. The dates (the bottom scale) are for weeks ending on that date for which normals and departures from normal were recorded. The P_01 to P_09 lines are the percentiles (10th to 90th) of all districts in every week.

And so we have an agricultural meteorology system that faithfully and reliably informs ‘kisans’ and cultivators in 641 districts what to expect from the weather for the next week. Thanks to mobile phones, weather alerts and crop advisories are distributed in all our major languages to a portion of the farming households working on 138 million farm holdings, (of which 117 million are small). But this is still only a portion, and is far from adequate in distributing the results of the work of our earth scientists and field staff.

Moreover, every other sector of development requires such raw data and location-specific analysis: the Department of Rural Development, the National Rural Health Mission, the Nirmal Bharat Abhiyan (for drinking water and sanitation), the food-based programmes (like the mid-day meals) for which the availability of ingredients and their supply is the essence of their work, the Central Water Commission and the Central Ground Water Board, whose work it is to determine the water flows and balances in river sub-basins and watersheds (there are 3,257), and districts administrations (which administer 232,855 panchayats) and municipal councils alike which must implement relief measures when drought sets in or must ration supply when there are shortages. This is but a small list of agencies whose work is directly affected by the Indian summer monsoon and its activity where they work.

A dense network of weather stations (more of these are being automated every month, but every taluka still does not have one) is complemented by dedicated satellites which provides continuous coverage of the sub-continent, the northern Asian land mass, the surrounding oceans southwards until beyond the Tropic of Capricorn.

The typical IMD map of 'normal' rainfall measured by the meteorological sub-divisions. The detailed weekly tables give us a very different picture

The typical IMD map of ‘normal’ rainfall measured by the meteorological sub-divisions. The detailed weekly tables give us a very different picture

Methods to simply and accurately funnel this stream of real-time data and imagery are available, mostly at no cost, in order to aid local administrations, farmers and cultivators, and all citizens. It is this availability and relative simplicity of use (block-level weather forecasts for 72 hours are now available as local language apps on smartphones) that must be encouraged by the official agencies – for they simply do not have the persons to do so at the scale and detail required.

Consider the setting in early July 2014. India’s summer monsoon was already late, and where it was late but active it was weak (as shown by the chart). The indications from the central earth science agencies (including the India Meteorological Department), from the Indian Institute of Tropical Meteorology, from the National Centre for Medium Range Weather Forecasting were that it would be end-June before the summer monsoon system settles over central India and the western Gangetic plains. This did not happen for another two weeks, until six of the usual 16 monsoon weeks had passed.

When in mid-July more rainfall was recorded in the districts, even then, as the chart shows, only 50% of the districts reached their ‘normals’ for that week only. Thereafter, the volatility of rainfall set in and while for those in our towns and cities there was relief from the searing summer temperatures the rains did not assure sowing conditions for farmers and cultivators, nor did it add, in July, to the stores of water in major and minor reservoirs.

That is why the IMD’s outdated and stodgy public outreach practice must be overhauled, completely. The bland map (see example) of sub-divisions is of little use when what we want to know pertains to tehsil and town. The Met Department’s rain adequacy categories must be replaced too by measures that are geared towards aiding alerts and advisories – ‘normal’ is rainfall up to +19% above a given period’s average and also down to -19% from that same average, a range that can make or break the efforts of a horticulturist.

This table illustrates the trend of weekly rainfall in 40 districts. These districts are selected as being home to the largest rural populations, two from the 20 major states (by population). The numbers by week and district describe how far from a 'normal' the recorded rainfall for that week was. Several overall observations stand out. Districts with weeks coloured light rose dominate, for these show those that received much less rain than they should have. Districts with a shade of deeper blue are the next most frequent category, and those received excess rain. Taken together, this tells us that extremes - very much less or more - were common for this group of districts in India with large rural populations. We can see the prolonged dry spells for districts in Haryana and Punjab; likewise the absence of rain for the first six monsoon weeks in Gujarat and Maharashtra; are examples of wide swings around weekly 'normal' in Giridih (Jharkhand), Muzaffarpur (Bihar), Haridwar (Uttarakhand), Mandi (Himachal Pradesh), Viluppuram (Tamil Nadu), and Mahbubnagar (Andhra Pradesh). The weeks ending 20 August in Bihar and the weeks ending September 3 and 10 in Jammu and Kashmir immediately stand out - the Kosi had breached its banks in Bihar and the Chenab submerged Srinagar and Jammu.

This table illustrates the trend of weekly rainfall in 40 districts. These districts are selected as being home to the largest rural populations, two from the 20 major states (by population). The numbers by week and district describe how far from a ‘normal’ the recorded rainfall for that week was.
Several overall observations stand out. Districts with weeks coloured light rose dominate, for these show those that received much less rain than they should have. Districts with a shade of deeper blue are the next most frequent category, and those received excess rain. Taken together, this tells us that extremes – very much less or more – were common for this group of districts in India with large rural populations.
We can see the prolonged dry spells for districts in Haryana and Punjab; likewise the absence of rain for the first six monsoon weeks in Gujarat and Maharashtra; are examples of wide swings around weekly ‘normal’ in Giridih (Jharkhand), Muzaffarpur (Bihar), Haridwar (Uttarakhand), Mandi (Himachal Pradesh), Viluppuram (Tamil Nadu), and Mahbubnagar (Andhra Pradesh). The weeks ending 20 August in Bihar and the weeks ending September 3 and 10 in Jammu and Kashmir immediately stand out – the Kosi had breached its banks in Bihar and the Chenab submerged Srinagar and Jammu.

Likewise, excess is +20% and more, deficient is -20% to -59% and scanty is -60% to -99%. To illustrate how misleading these categories can be, the difference between an excess of +21% and +41% can be the difference between water enough to puddle rice fields and a river breaking its banks to ruin those fields. [Get a full resolution image of the table here, 1.85 MB.]

The yawning gap between the technical competence of India’s climate monitoring systems, and they ways in which they are used, must be bridged and this is best done through public participation and citizen initiative. The politics of monsoon and of water will continue, but must not be allowed to define how our systems are used. Nor must they detract from our long history of weather observation, which dates back at least to the ‘Vrhat Sanhita’ of Varahamihira.

It has only signalled policy confusion for central and state governments to have not declared districts and talukas as affected by drought – which they should have by late July 2014 – while at the same time quietly announcing to administrations, as the Ministry of Agriculture did, that “to deal with challenges posed by delayed and aberrant monsoon and in the wake of shortfall in sowing of major crops during kharif 2014, the government has initiated interventions”. These being a diesel subsidy for what is called ‘protective irrigation’ of crops, raising the ceiling on the seed subsidy, rolling out a drought mitigating programme for horticulture, boosting fodder cultivation through the flagship Rashtriya Krishi Vikas Yojana.

The new government has stated time and again its desire to improve and strengthen governance. This must come to include a concerted drive to democratise the use of public domain information, including our monsoon and water, in order that we residents of 4,041 statutory towns (large cities included) and 3,894 census towns can judge for ourselves the relationships between the food we buy, they rain we receive, our individual use of about 70 litres of water a day, and the fluctuation of these trends from one monsoon to another. The moral of monsoon 2014 is that we must reclaim local measures for local use.

Rahul Goswami

Filed Under: Latest, Monsoon 2014 Tagged With: 2014, administration, agriculture, crop, district, ground water, health, IMD, India, krishi, meteorology, monsoon, policy, remote sensing, river, sanitation, smartphone, varahamihira, vrhat samhita, water, watershed, weather station

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